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LITHOLOGY AND SEDIMENTATION CONDITIONS OF PALEOCENE DEPOSITS OF THE SOUTH SLOPE OF THE KARKINITE DEPRESSION (BLACK SEA COAST)

Home > Archive > No. 1–2 (187–188) 2022 > 71–81

Geology & Geochemistry of Combustible Minerals No. 1–2 (187–188) 2022, 71–81.

https://doi.org/10.15407/ggcm2022.01-02.071

Kostyantyn HRYGORCHUK1, Volodymyr HNIDETS2, Lina BALANDYUK

Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, Ukraine, e-mail: 1kosagri@ukr.net; 2vgnidets53@gmail.com

Abstract

According to the results of lithological studies of the Paleocene sediments of the southern side of the Karkinite Depression, the lateral lithological-lithmological and facial variability of the sediments is characterized, which is manifested both in the whole section of the Paleocene and its individual epochs. It is shown that the role of limestone formations clearly decreases from the beginning to the end of the period with their maximum development in Zealand time. Sediments of the Tanetian epoch are characterized by dominance in the section of marl-clay formations and the development of siltstone-sand bodies in the area of the Odesa structure. Sediments are represented by three types of section: terrigenous (well Odeska-2), carbonate (wells Hamburtseva-2, Selskogo-40), carbonate-clay (wells Crimean-1, Shtormova-5, Centralna-1, Arkhangelskogo-1). In different areas, each type of section is characterized by a certain specificity of the internal structure. Lithological heterogeneity of sediments is associated with spatial and age variability of biofacial zones: biogerms, inland biogerm lagoons, plumes of destruction of bioherms, the outer shelf. In the sediments of the Danian age, small limestone bodies are localized in the Shtormova and Odesa structures. Zealand strata in the area from well Hamburtseva-2 to well Centralna-1 are characterized by significant development of bioherms, which are replaced in the direction of the Odesa structure by plumes of destruction and sediments of basin plains. The development of bioherm formations in the axial part of the depression is predicted, which is associated with the sedimentary manifestation of the Central Mikhailovsky uplift. This significantly expands the prospects for oil and gas in this part of the study area. During the Tanetian period, rising sea levels caused an increase in the area of distribution of the outer shelf in the axial zone of depression. At the same time, in the area of the structures of Hamburtseva, Selskogo, Centralna inheritedly (despite the transgression) were developed biohermic massifs, which was caused by upward movements within the Black Sea-Kalamitsky uplift.

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Keywords

lithology, facies, sedimentation conditions, Paleocene, Karkinite Depression

Referenses

Fortunatova, N. K. (Ed.). (2000). Sedimentologicheskoe modelirovanie karbonatnikh osadochnikh kompleksov [Sedimentological modeling of carbonate sedimentary complexes]. Moskva: REFIA. [in Russian]

Gromin, V. I., Rogoza, O. I., Chaitskii, V. P., & Shimanskii, A. A. (1986). Klinoformi severo-zapadnogo shelfa Chernogo morya, ikh genezis i usloviya neftegazonosnosti [Clinoforms of the northwestern shelf of the Black Sea, their genesis and conditions of oil and gas potential]. Geologiya nefti i gaza, 10, 46–53. [in Russian]

Hnidets, V. P., Hryhorchuk, K. H., & Balandiuk, L. V. (2021). Osoblyvosti formuvannia nyzhnokreidovoi tektono-sedymentatsiinoi systemy Prychornomorskoho mehaprohynu [Peculiarities of formation of the Lower Cretaceous teсtono-sedimentation system of the Black Sea megadepression]. Heolohichnyi zhurnal, 2(375), 67–78. https://doi.org/10.30836/igs.1025-6814.2021.2.224399 [in Ukrainian]

Hnidets, V. P., Hryhorchuk, K. H., Kurovets, I. M., Kurovets, S. S., Prykhodko, O. A., Hrytsyk, I. I., & Balandiuk, L. V. (2013). Heolohiia verkhnoi kreidy Prychornomorsko-Krymskoi naftohazonosnoi oblasti (heolohichna paleookeanohrafiia, litohenez, porody-kolektory i rezervuary vuhlevodniv, perspektyvy naftohazonosnosti) [Geology of the Upper Cretaceous of the Black Sea-Crimean oil and gas region (geological paleoceanography, lithogenesis, reservoir rocks and hydrocarbon reservoirs, oil and gas potential)]. Lviv: Poli. [in Ukrainian]

Hozhyk, P. F. (Ed.). (2006). Stratyhrafiia mezokainozoiskykh vidkladiv pivnichno-zakhidnoho shelfu Chornoho moria [Stratigraphy of Mesocainozoic sediments of the north-western shelf of the Black Sea]. Kyiv. [in Ukrainian]

Ilin, V. D., & Fortunatova, N. K. (1988). Metodi prognozirovaniya i poiskov neftegazonosnikh rifovikh kompleksov [Methods of forecasting and searching for oil and gas reef complexes]. Moskva: Nedra. [in Russian]

Karogodin, Yu. N. (1980). Sedimentatsionnaya tsiklichnost [Sedimentation cycle]. Moskva: Nedra. [in Russian]

Kozlenko, M. V., Kozlenko, Yu. V., & Lisinchuk, D. V. (2013). Struktura zemnoi kori severo-zapadnogo shelfa Chernogo morya vdol profilya GSZ No. 26 [The structure of the earth’s crust in the N-W of the Black Sea shelf along the DSS profile No. 26]. Heofizychnyi zhurnal, 35(1), 142–152. https://doi.org/10.24028/gzh.0203-3100.v35i1.2013.116345 [in Russian]

Rever, V. B. (2016). Litohenez eotsenovykh vidkladiv Chornomorskoho sehmentu okeanu Tetis [Lithogenesis of Eocene sediments of the Black Sea segment of the Tethys Ocean]. Kyiv: Naukova dumka. [in Ukrainian]

Vail, P. R., Mitchum Jr., R. M., & Thompson III, S. (1977). Seismic stratigraphy and global changes of sea level: Part 4. Global cycles of relative changes of sea level. AAPG, Memoir, 26, 83–97. https://doi.org/10.1306/M26490C6

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LITHOGEOCHEMISTRY OF BLACK SHALES OF THE PHANEROZOIC OF THE WESTERN UKRAINE – UNCONVENTIONAL HYDROCARBON RESERVOIRS

Home > Archive > No. 1–2 (187–188) 2022 > 82–102

Geology & Geochemistry of Combustible Minerals No. 1–2 (187–188) 2022, 82–102.

https://doi.org/10.15407/ggcm2022.01-02.082

Ihor POPP, Petro MOROZ, Mykhaylo SHAPOVALOV

Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, Ukraine, e-mail: itpopp@ukr.net

Abstract

The purpose of this work is to compare the lithological, geochemical and mineralogical features of carbonaceous clayey and siliceous-clay rocks of Cretaceous-Paleogene flysch of the Ukrainian Carpathians and Lower Silurian of the Volyn-Podillya edge of the East European Platform and to determine the factors that contributed to the formation of zones of “unconventional reservoirs” in these sedimentary strata of cracked and mixed types.

Data from the lithology, geochemistry and mineralogy of bituminous siliceous-clay rocks and siliceous rocks of Lower Cretaceous and Oligocene of the Carpathians and black argillites of Lower Silurian of the Volyn-Podillya edge of the East European Platform are presented.

Sedimentogenesis of Lower Cretaceous and Oligocene bituminous deposits of the Carpathians and Lower Silurian deposits of Volyn-Podillya took place in anoxic conditions (phases of oceanic anoxic events: OAE-1 (Barrem–Albian), OAE-4 (Oligocene) and at the border of Ordovician and Silurian. Paleoceanographic conditions of their sedimentation differed significantly. The first are deep-sea formations at the foot of the continental slope of the Carpathian segment of the Tethys Ocean, the second were accumulated in the warm shallow sea on the eastern shelf of the West European Sea Basin.

The layered texture of carbonaceous deposits, as well as the catagenetic transformation of rock-forming clay and siliceous minerals and their hydrophobization, played a significant role in the formation of the filtration capacity properties of “unconventional reservoirs”. In Cretaceous-Paleogene flysch deposits of the Carpathians, “unconventional reservoirs” are usually terrigenous-clay or siliceous-clay rocks with shale and layered texture or compacted sandstones localized in conventional oil, gas or condensate deposits. Lower Silurian clay deposits of Volyn-Podillya are promising for the search for “shale gas”.

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Keywords

unconventional reservoirs, black shales, shale gas, clay minerals, organic carbon

Referenses

Afanaseva, I. M. (1983). Litogenez i geokhimiya flishevoi formatsii severnogo sklona Sovetskikh Karpat. Kiev: Naukova dumka. [in Russian]

Beckwith, R. (2013). California’s Monterey Formation Zeroing in on a New Shale Oil Play? J. Pet. Technol., 5, (65), 44–58. https://doi.org/10.2118/0513-0044-JPT

Behl, R. J. (2011). Chert spheroids of the Monterey Formation, California (USA): early-diagenetic structures of bedded siliceous deposits. Sedimentology, 58, 325–351. https://doi.org/10.1111/j.1365-3091.2010.01165.x

Bratcher, J. C., Kaszuba, J. P., Herz-Thyhsen, R. J., & Dewey, J. C. (2021). Ionic strength and pH effects on water–rock interaction in an unconventional siliceous reservoir: on the use of formation water in hydraulic fracturing. Energy Fuels, 35(22), 18414–18429. https://doi.org/10.1021/acs.energyfuels.1c02322

Cipolla, C. L., Lolon, E. P., Erdle, J. C., & Rubin, B. (2010). Reservoir Modeling in Shale-Gas Reservoirs. SPE Res Eval & Eng, 13(04), 638–653. https://doi.org/10.2118/125530-PA

Curtis, J. B. (2002). Fractured shale-gas systems. AAPG Bulletin, 86(11), 1921–1938. https://doi.org/10.1306/61EEDDBE-173E-11D7-8645000102C1865D

Gabinet, M. P. (1985). Postsedimentatsionnie preobrazovaniya flisha Ukrainskikh Karpat. Kiev: Naukova dumka. [in Russian]

Gabinet, M. P., & Gabinet, L. M. (1991). K geokhimii organicheskogo veshchestva bituminoznikh argillitov flishevoi formatsii Karpat. Geologiya i geokhimiya goryuchikh iskopaemikh, 76, 23–31. [in Russian]

Gabinet, M. P., Kulchitskii, Ya. O., & Matkovskii, O. I. (1976). Geologiya i poleznie iskopaemie Ukrainskikh Karpat (Part 1). Lvov: Izdatelstvo Lvovskogo universiteta. [in Russian]

Gurzhii, D. V., Gabinet, M. P., Kiselev A. Ye. i dr. (1983). Litologiya i porodi-kollektori na bolshikh glubinakh v neftegazonosnikh provintsiyakh. Kiev: Naukova dumka. [in Russian]

Hryhorchuk, K. H., & Senkovskyi, Yu. M. (2013). Dyskretne formuvannia rezervuariv “slantsevoho” hazu v eksfiltratsiinomu katahenezi. Heodynamika, 1(14), 61‒67. https://doi.org/10.23939/jgd2013.01.061 [in Ukrainian]

Hubych, I., Krupskyi, Yu., Lazaruk, Ya., & Syrota, T. (2012). Aktualni aspekty heolohii ta heokhimii slantsevoho hazu Volyno-Podillia. Heoloh Ukrainy, 1‒2, 135‒140. [in Ukrainian]

Isaacs, C. M. (1984). Geology and Physical Properties of the Monterey Formation, California. In SPE California Regional Meeting. SPE-12733-MS. Society of Petroleum Engineers. https://doi.org/10.2118/12733-MS

Jiang, S. (2012). Clay Minerals from the Perspective of Oil and Gas Exploration. In M. Valaškova, & G. S. Martynkova (Eds.), Clay Minerals in Nature – Their Characterization, Modification and Application. IntechOpen. https://doi.org/10.5772/47790

Klubova, T. T. (1988). Glinistie kolektori nefti i gaza. Moskva: Nedra. [in Russian]

Kolodii, V. V., Boiko, H. Yu., Boichevska, L. T., Bratus, M. D., Velychko, N. Z., Harasymchuk, V. Yu., Hnylko, O. M., Danysh, V. V., Dudok, I. V., Zubko, O. S., Kaliuzhnyi, V. A., Kovalyshyn, Z. I., Koltun, Yu. V., Kopach, I. P., Krupskyi, Yu. Z., Osadchyi, V. H., Kurovets, I. M., Lyzun, S. O., Naumko, I. M., . . . Shcherba, O. S. (2004). Karpatska naftohazonosna provintsiia. Lviv; Kyiv: Ukrainskyi vydavnychyi tsentr. [in Ukrainian]

Koltun, Yu. V. (1993). Source rock potential of the black formation of the Ukrainian Carpathians. Acta Geologica Hungarica, 2(36), 251–261.

Kondrat, О. R., & Hedzyk, N. M. (2014). Study of adsorption processes influence on development of natural gas fields with low permeability reservoirs. Rozvidka ta rozrobka naftovykh i hazovykh rodovyshch, 4(53), 7‒17.

Kosakowski, P., Koltun, Yu., Machowski, G., Poprawa, P., & Papiernik, B. (2018). The geochemical characteristics of the Oligocene – Lower Miocene Menilite Formation in the Polish and Ukranian Outer Carpathians: a review. Journal of Petroleum Geology, 41(3), 319–335. https://doi.org/10.1111/jpg.12705

Krupskyi, Yu. Z., Kurovets, I. M., Senkovskyi, Yu. M., Mykhailov, V. A., Chepil, P. M., Dryhant, D. M., Shlapinskyi, V. S., Koltun, Yu. V., Chepil, V. P., Kurovets, S. S., & Bodlak, V. P. (2014). Netradytsiini dzherela vuhlevodniv Ukrainy: Vol. 2. Zakhidnyi naftohazonosnyi rehion. Kyiv: Nika-Tsentr. [in Ukrainian]

Kukhar, N. P., Petrovskyi, O. P., & Hanzhenko, N. S. (2013). Zastosuvannia heofizychnykh metodiv dlia poshukiv, rozvidky i rozrobky pryrodnoho hazu zi slantsevykh porid. Heodynamika, 2(15), 195‒197. https://doi.org/10.23939/jgd2013.02.195 [in Ukrainian]

Kurovets, I. M., Mykhailov, V. A., Zeikan, O. Yu., Krupskyi, Yu. Z., Hladun, V. V., Chepil, P. M., Hulii, V. M., Kurovets, S. S., Kasianchuk, S. V., Hrytsyk, I. I., & Naumko, I. M. (2014). Netradytsiini dzherela vuhlevodniv Ukrainy: Vol. 1. Netradytsiini dzherela vuhlevodniv: ohliad problemy. Kyiv: Nika-Tsentr. [in Ukrainian]

Kurovets, S. S. (2016). Naukovo-metodychni zasady otsinky vtorynnykh yemnostei porid-kolektoriv yak osnova efektyvnoho prohnozu naftohazonosnosti nadr [Extended abstract of Doctorʼs thesis]. Ivano-Frankivsk. [in Ukrainian]

Liehui, Z., Baochao, S., Yulong, Z., & Zhaoli, G. (2019). Review of micro seepage mechanisms in shale gas reservoirs. International Journal of Heat and Mass Transfer, 139, 144‒179. https://doi.org/10.1016/j.ijheatmasstransfer.2019.04.141

Loktiev, A. V., Pavliuk, M. I., & Loktiev, A. A. (2011). Perspektyvy vidkryttia pokladiv “slantsevoho“ hazu v mezhakh Volyno-Podilskoi okrainy Skhidno-Yevropeiskoi platformy. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4(156–157), 5–23. [in Ukrainian]

Loucks, R. G., Reed, R. M., Ruppel, S. C., & Jarvie, D. M. (2009). Morphology, genesis, and distribution of nanometer-scale pores in siliceous mudstones of the Mississippian Barnet shale. Journal of Sedimentary Research, 79(12), 848–861. http://doi.org/10.2110/jsr.2009.092

Lukin, A. Ye. (2010a). Slantsevii gaz i perspektivi yego dobichi v Ukraine. Statya 1. Sovremennoe sostoyanie problemi slantsevogo gaza (v svete opita osvoeniya yego resursov v SShA). Heolohichnyi zhurnal, 3, 17–33. https://doi.org/10.30836/igs.1025-6814.2010.3.219195 [in Russian]

Lukin, A. Ye. (2010b). Slantsevii gaz i perspektivi yego dobichi v Ukraine. Statya 2. Chernoslantsevie kompleksi Ukraini i perspektivi ikh gazonosnosti v Volino-Podolii i Severo-Zapadnom Prichernomore. Heolohichnyi zhurnal, 4, 7–24. https://doi.org/10.30836/igs.1025-6814.2010.4.215055 [in Russian]

Lukin, A. Ye. (2011a). O prirode i perspektivakh gazonosnosti nizkopronitsaemikh porod osadochnoi obolochki Zemli. Dopovidi NAN Ukrainy, 3, 114–123. [in Russian]

Lukin, A. Ye. (2011b). Priroda slantsevogo gaza v kontekste problem neftegazovoi litologii. Geologiya i poleznie iskopaemie Mirovogo okeana, 3, 70–85. [in Russian]

Lukin, A. Ye. (2016). O novikh geneticheskikh tipakh porod litosferi – vazhneishikh faktorakh formirovaniya kollektorov nefti i gaza. Tektonika i stratyhrafiia, 43, 5‒18. https://doi.org/10.30836/igs.0375-7773.2016.108272 [in Russian]

Monchak, L., Khomyn, V., Maievskyi, B., Shkitsa, L., Kurovets, S., Zderka, T., & Stasyk, I. (2013). Haz sharuvatykh nyzkoporystykh verkhnokreidovykh porid (slantsevyi haz) Skybovykh Karpat. Heoloh Ukrainy, 1(141), 56‒62. https://doi.org/10.53087/ug.2013.1(41).246559 [in Ukrainian]

Naumko, I. M., Kurovets, I. M., Zubyk, M. I., Batsevych, N. V., Sakhno, B. E., & Chepusenko, P. S. (2017). Hydrocarbon compounds and plausible mechanism of gas generation in “shale” gas prospective Silurian deposits of Lviv Paleozoic depression. Heodynamika, 1(22), 26–41. https://doi.org/10.23939/jgd2017.01.036

Nesterov, I. I., Ushatinskii, I. N., Malikhin, A. Ya., Stavitskii, B. P., & Pyankov, B. N. (1987). Neftenosnost glinistikh tolshch Zapadnoi Sibiri. Moskva: Nedra. [in Russian]

Passey, Q. R., Bohacs, K. M., Esch, W. L., Klimentidis, R., & Sinha, S. (2010). From Oil-Prone Source Rock to Gas-Producing Shale Reservoir – Geologic and Petrophysical Characterization of Unconventional Shale-Gas Reservoirs. In CPS/SPE International Oil & Gas Conference and Exhibition in China held in Beijing, China, 8–10 June 2010. SPE 131350. Society of Petroleum Engineers. https://doi.org/10.2118/131350-MS

Popp, I. T. (1995). Naftomaterynski vlastyvosti bituminoznykh kremenystykh vidkladiv Ukrainskykh Karpat. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4, (92–93), 35–41. [in Ukrainian]

Popp, I. T. (2005). Okremi aspekty problemy litohenezu naftohazonosnykh vidkladiv kreidovo-paleohenovoho flishovoho kompleksu Peredkarpatskoho prohynu ta ukrainskykh Karpat. Chastyna 1. Sedymentohenez i postsedymentatsiini peretvorennia. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4, 43–59. [in Ukrainian]

Popp, I., Moroz, P., & Shapovalov, M. (2019). Litoloho-heokhimichni typy kreidovo-paleohenovykh vidkladiv Ukrainskykh Karpat ta umovy yikhnoho formuvannia. Heolohiia i heokhimiia horiuchykh kopalyn, 4(181), 116‒133. https://doi.org/10.15407/ggcm2019.04.116 [in Ukrainian]

Popp, I., Shapovalov, M., & Moroz, P. (2018). Mineralohichnyi ta heokhimichnyi aspekt problemy slantsevoho hazu (na prykladi chornykh arhilitiv zakhodu Ukrainy). Mineralohichnyi zbirnyk, 1(68), 184–186. [in Ukrainian]

Popp, I. T., Shapovalov, M. V., & Moroz, P. V. (2019). Chorni arhility zakhodu Ukrainy yak potentsiini porody-kolektory (mineraloho-heokhimichnyi aspekt problemy “slantsevoho hazu”). In Heolohiia horiuchykh kopalyn: dosiahnennia ta perspektyvy: materialy III Mizhnarodnoi naukovoi konferentsii (pp. 42–47). Kyiv. [in Ukrainian]

Rauball, J. F., Sachsenhofer, R. F., Bechtel, A., Coric, S., & Gratzer, R. (2019). The Oligocene‒Miocene Menilite Formation in the Ukrainian Carpathians: a world-class source rock. Journal of Petroleum Geology, 42(4), 393‒415. https://doi.org/10.1111/jpg.12743

Ross, D. J. K., & Bustin, R. M. (2009). The importance of shale composition and pore structure upon gas storage potential of shale gas reservoirs. Marine and Petroleum Geology, 26(6), 916–927. http://doi.org/10.1016/j.marpetgeo.2008.06.004

Rudko, H. I., Hryhil, H. V., & Simachenko, H. V. (2017). Ekolohichna bezpeka rodovyshch vuhlevodniv netradytsiinoho typu v Ukraini. Kyiv; Chernivtsi: Bukrek. [in Ukrainian]

Samvelov, R. G. (1995). Zalezhi uglevodorodov na bolshikh glubinakh: osobennosti formirovaniya i razmeshcheniya. Geologiya nefti i gaza, 9, 5–15. [in Russian]

Schwalbach, J. R., Gordon, S. A., O’Brien, C. P., Lockman, D. F., Benmore, W. C., Huggins, C. A. (2009). Reservoir characterization Monterey Formation siliceous shales: tools and applications. In Contributions to the Geology of the San Joaquin Basin, California. Pacific Section American Association of Petroleum Geologists. MP 48. https://doi.org/10.32375/2009-MP48.7

Senkovskyi, Yu., Hryhorchuk, K., Hnidets, V., & Koltun, Yu. (2004). Heolohichna paleookeanohrafiia okeanu Tetis (Karpato-Chornomorskyi sehment). Kyiv: Naukova dumka. [in Ukrainian]

Senkovskyi, Yu. M., Hryhorchuk, K. H., Koltun, Yu. V., Hnidets, V. P., Radkovets, N. Ya., Popp, I. T., Moroz, M. V., Moroz, P. V., Rever, A. O., Haievska Yu. P., Havryshkiv, H. Ya., Kokhan, O. M., & Koshil, L. B. (2019). Litohenez osadovykh kompleksiv okeanu Tetis. Karpato-Chornomorskyi sehment. Kyiv: Naukova dumka. [in Ukrainian]

Senkovskyi, Yu. M., Koltun, Yu. V., Hryhorchuk, K. H., Hnidets, V. P., Popp, I. T., & Radkovets, N. Ya. (2012). Bezkysnevi podii okeanu Tetis. Karpato-Chornomorskyi sehment. Kyiv: Naukova dumka. [in Ukrainian]

Tisso, B., & Velte, D. (1981). Obrazovanie i rasprostranenie nefti. Moskva: Mir. [in Russian]

Visotskii, I. V., & Visotskii, V. I. (1986). Formirovanie neftyanikh, gazovikh i kondensatnogazovikh mestorozhdenii. Moskva: Nedra. [in Russian]

Vyalov, O. S., Gavura, S. P., Danish, V. V., Lemishko, O. D., Leshchukh, R. I., Ponomareva, L. D., Romaniv, A. M., Smirnov, S. Ye., Smolinskaya, N. I., & Tsarnenko, P. N. (1988). Stratotipi melovikh i paleogenovikh otlozhenii Ukrainskikh Karpat. Kiev: Naukova dumka. [in Russian]

Vyalov, O. S., Gavura, S. P., Danish, V. V., Leshchukh, R. I., Ponomareva, L. D., Romaniv, A. M., Tsarnenko, P. N., & Tsizh, I. T. (1981). Istoriya geologicheskogo razvitiya Ukrainskikh Karpat. Kiev: Naukova dumka. [in Russian]

Wilson, M. J., Shaldybin, M. V., & Wilson, L. (2016). Clay mineralogy and unconventional hydrocarbon shale reservoirs in the USA. I. Occurrence and interpretation of mixed-layer R3 ordered illite/smectite. Earth-Science Reviews, 158, 31‒50. https://doi.org/10.1016/j.earscirev.2016.04.004

Yan, B., Alfi, M., Wang, Y., & Killough, J. E. (2013). A New Approach for the Simulation of Fluid Flow in Unconventional Reservoirs through Multiple Permeability Modeling. In SPE Annual Technical Conference and Exhibition held in New Orleans, Louisiana, USA, 30 September–2 October 2013. SPE 166173. https://doi.org/10.2118/166173-MS

Yevdoshchuk, M. I., & Bondar, H. M. (2019). Prohnozuvannia porid-kolektoriv v hlybokozanurenykh horyzontakh. In Heolohiia horiuchykh kopalyn: dosiahnennia ta perspektyvy: materialy III Mizhnarodnoi naukovoi konferentsii (pp. 69–73). Kyiv. [in Ukrainian]

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GEOCHEMICAL FEATURES OF STRONTIUM ACCUMULATION AND MIGRATION IN THE PEATS OF THE LVIV REGION

Home > Archive > No. 1–2 (187–188) 2022 > 58–70

Geology & Geochemistry of Combustible Minerals No. 1–2 (187–188) 2022, 58–70.

https://doi.org/10.15407/ggcm2022.01-02.058

Myroslava YAKOVENKO

Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, Ukraine, e-mail: myroslavakoshil@ukr.net

Abstract

The article is devoted to the study of geochemical characteristics of the distribution, accumulation and migration of strontium in the lowland peats of the Lviv Region, both laterally and vertically, and to identify the main factors influencing the formation of its concentrations.

A significant uneven distribution of concentration, high dispersion and variability (coefficient of variation – 116.61, standard deviation – 564.11) of Sr in peats within deposits, districts and regions both with depth and area of distribution and high content indicators were established Sr relative to clarks of the lithosphere, soils, plant ash (CC relative to the lithosphere = 1.42; CC relative to soil clarks = 1.94; Сs relative to background values in the soils of Ukraine = 4.56; CK relative to clarks of terrestrial plants = 1.61).

The content of Sr in the peat of the Lviv Region ranges from 40–3190 mg/kg (average content 483.75 mg/kg, median content (background content) – 250 mg/kg), which is due to natural-climatic, geological, lithological, hydrogeochemical and anthropogenic factors.

The features of the distribution and the degree of concentration of Sr in the peatlands of the Lviv Region are mainly influenced by the chemical-mineralogical-petrographic composition of the bedrocks of the wear area during their weathering; terrain, climatic, geomorphological, tectonic and hydrogeological conditions of the area, which determine the of the weathering processes of the rocks in the wear areas, the degree of transformation of terrigenous material in the weathering processes, the rate of accumulation of biomass and the rate of its decomposition; features of water and mineral nutrition of the peatland.

High concentrations of strontium in the peat of the Lviv Region reflect the local regional processes of the concentration of the element in the mass of peat and may indicate the accumulation of Sr of both natural and anthropogenic origin in the upper layers of peat profiles. There is an enrichment of Sr in the upper intervals of deposits (0–1 m) of deposits in the northeastern part of the Lviv Region (Malopoliska peat region) is observed.

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Keywords

peat, peat deposit, strontium, microelement composition, concentration, Clark concentration, accumulation, migration

Referenses

Angino, E., Billings, G. K., & Andersen, N. (1966). Observed variations in the strontium concentration of seawater. Chemical Geology, 1, 145–153. https://doi.org/10.1016/0009-2541(66)90013-1

Boiko, T. I. (1995). Heokhimiia sirky ta strontsiiu v zoni tekhnohenezu sirkodobuvnykh pidpryiemstv Peredkarpattia [Extended abstract of Candidateʼs thesis]. Instytut heolohii i heokhimii horiuchykh kopalyn NAN Ukrainy. Lviv. [in Ukrainian]

Bowen, H. J. M. (1979). Environment Chemistry of the Elements. London; New-York; Toronto; Sydney; San-Francisco: Academic Press.

Buchynska, I., Lazar, H., Savchynskyi, L., & Shevchuk, O. (2013). Umovy utvorennia vuhillia plasta n8 Lvivsko-Volynskoho baseinu za heokhimichnymy danymy. Heolohiia i heokhimiia horiuchykh kopalyn, 1–2, 32–41. [in Ukrainian]

Burkov, V. V., & Podporina, Ye. K. (1962). Strontsii. Trudi Instituta mineralogii, geokhimii i kristallografii redkikh metallov, 12, 180. [in Russian]

Chertko, N. K., & Chertko, E. N. (2008). Geokhimiya i ekologiya khimicheskikh elementov. Minsk: Izdatelskii tsentr BGU. [in Russian]

For, G., & Dzhons, L. (1974). Izotopnii sostav strontsiya v rossipyakh Krasnogo morya. In Sovremennoe gidrotermalnoe rudootlozhenie (pp. 141–148). Moskva: Mir. [in Russian]

Ivantsiv, O. Ye., & Uzhenkov, G. A. (1984). Geokhimicheskie osobennosti torfyano-bolotnogo litogeneza Prikarpatya. In Osadochnie porodi i rudi (pp. 215–220). Kiev: Naukova dumka. [in Russian]

Kabata-Pendias, A., & Pendias, X. (1989). Mikroelementi v pochvakh i rasteniyakh. Moskva: Mir. [in Russian]

Klos, V. R., Birke, M., Zhovynskyi, E. Ya., Akinfiiev, H. O., Amaiyukeli, Yu. A., & Klamens, R. (2012). Rehionalni heokhimichni doslidzhennia gruntiv Ukrainy v ramkakh mizhnarodnoho proektu z heokhimichnoho kartuvannia silskohospodarskykh ta pasovyshchnykh zemel Yevropy (GEMAS). Poshukova ta ekolohichna heokhimiia, 1, 51–66. [in Ukrainian]

Kushnir, S. V., Shuter, Ya. N., Pankiv, R. II., & Srebrodolskii, B. I. (1982). Osnovnie formi nakhozhdeniya strontsiya v sernikh rudakh Predkarpatya. In Geologiya i geokhimiya nemetallicheskikh iskopaemikh (pp. 102–108). Kiev: Naukova dumka. [in Russian]

Kushnir, S. V., Vivchar, O. I., & Boiko, T. I. (1995). Deiaki heokhimichni naslidky zastosuvannia “vapniakovo-sirchanoho dobryva”. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4(88–89), 27–35. [in Ukrainian]

Kyrylchuk, A. A., & Bonishko, O. S. (2011). Khimiia gruntiv. Osnovy teorii i praktykum. Lviv: LNU imeni Ivana Franka. [in Ukrainian]

Lazar, H. (2017). Osoblyvosti poshyrennia strontsiiu u vuhilli plasta v6 Lvivsko-Volynskoho baseinu. Heolohiia i heokhimiia horiuchykh kopalyn, 1–2(170–171), 86. [in Ukrainian]

Noll, W. (1931). Über die Bestimmung des Strontiums in der Mineral- und Gesteinsanalyse. Zeitschrift für anorganische und allgemeine Chemie, 199(1), 193–208. https://doi.org/10.1002/zaac.19311990121

Odum, H. T. (1951). Notes on the Strontium Content of Sea Water, Celestite Radiolaria, and Strontianite Snail Shells. Science, 114(2956), 211–213. https://doi.org/10.1126/science.114.2956.211

Orru, H., & Orru, M. (2006). Sources and distribution of trace elements in Estonian peat. Global and Planetary Change, 53(4), 249–258. https://doi.org/10.1016/j.gloplacha.2006.03.007

Pampura, V. D., Sandimirova, G. P., & Brandt, S. B. (1991). Geokhimiya i izotopnii sostav strontsiya v gidrotermalnikh sistemakh. Nauka, Sibirskoe otdelenie. [in Russian]

Sklyarov, Ye. V., Barash, I. G., Bulanov, V. A., Gladkochub, D. P., Donskaya, T. V., Ivanov, A. V., Letnikova, Ye. F., Mironov, A. G., & Sizikh, A. I. (2001). Interpretatsiya geokhimicheskikh dannikh. Moskva: Intermetinzhiniring. [in Russian]

Sprynskyi, M. I. (1999). Litii, rubidii, tsezii i strontsii u pidzemnykh vodakh Karpatskoi naftohazonosnoi provintsii [Extended abstract of Candidateʼs thesis]. Instytut heolohii i heokhimii horiuchykh kopalyn NAN Ukrainy. Lviv. [in Ukrainian]

Turekian, K. K., & Kulp, J. L. (1956). The geochemistry of strontium. Geochimica et Cosmochimica Acta, 10(5–6), 245–296. https://doi.org/10.1016/0016-7037(56)90015-1

Voitkevich, G. V., Miroshnikov, A. Ye., Povarennikh, A. S., & Prokhorov, V. G. (1970). Kratkii spravochnik po geokhimii. Moskva: Nedra. [in Russian]

Yakovenko, M., Khokha, Yu., & Liubchak, O. (2022). Heokhimichni osoblyvosti nakopychennia i mihratsii vazhkykh metaliv u torfakh Lvivskoi oblasti. Visnyk Kharkivskoho natsionalnoho universytetu imeni V. N. Karazina, ceriia “Heolohiia. Heohrafiia. Ekolohiia”, 56, 105–121. https://doi.org/10.26565/2410-7360-2022-56-07 [in Ukrainian]

Yakovenko, M., Khokha, Yu., & Liubchak, O. (2021). Rozpodil khimichnykh elementiv u nyzynnykh torfakh Lvivskoi oblasti. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4(185–186), 65–72. https://doi.org/10.15407/ggcm2021.03-04.065 [in Ukrainian]

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DEFORMATIONS IN THE THRUST ZONE BETWEEN THE ZELEMIANKA AND PARASHKA SKYBAS OF THE UKRAINIAN CARPATHIAN SKYBA NAPPE (HREBENIV QUARRY)

Home > Archive > No. 1–2 (187–188) 2022 > 48–57

Geology & Geochemistry of Combustible Minerals No. 1–2 (187–188) 2022, 48–57.

https://doi.org/10.15407/ggcm2022.01-02.048

Milena BOGDANOVA

Ivan Franko National University of Lviv, Ukraine, e-mail: milena_bogdanova@ukr.net

Abstract

In the article, based on own field observations, the deformation structures into the thrust zone of the Zelemianka Skyba (=thrust-sheet) onto the Parashka Skyba (the Ukrainian Carpathian Skyba Nappe) are described. They are exposed in the Hrebeniv quarry located in the Opir River basin (Lviv Region, Skole district). The tectonically disintegrated Stryi Formation (Upper-Cretaceous–Paleocene flysch) characterized by the rigid sandstone blocks (formed mainly as a result of boudinage) placed in a ductile clay matrix is represented in the Hrebeniv quarry. This formation is proposed to be classified as a “broken formation”, which is strongly tectonized, but retain their lithological and stratigraphic identity. It is a transitional element between the weakly deformed strata and tectonic mélange. Their characteristic features are: linearity of the distribution zone; significant monomictic composition and absence of exotic formations; the presence of an intensively tectonized matrix with clastolites (blocks) of less tectonized rocks of the same lithostratum (formation, series); the presence of newly formed hydrothermal minerals in clastolite cracks; the upper and lower contacts limiting the broken formation have a tectonic nature. An intensely tectonized matrix and a weakly tectonized rigid blocks belong to the same stratigraphic unit in a broken formation. The structural features suggest a brittle deformations in the studied rocks. Tectonic processes occurred in the completely lithified deposits. Thrust processes were accompanied by the formation of the duplexes, including antiformal stack duplexes, which are well expressed in the quarry. Duplexes are observed in different parts of the quarry, and the most representative ones are developed in its central section. Horses in the duplexes are characterized by a size of 1 to 3 meters here. They are generally subparallel, which is consistent with monoclinal bedding, however, they sometimes acquire an antiform appearance as a result of tectonic thrusting.

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Keywords

Ukrainian Carpathians, Skyba Nappe, broken formation, thrust zone, deformations, duplexes

Referenses

Astakhov, K. P. (1989). Alpiiskaya geodinamika Ukrainskikh Karpat [Extended abstract of Candidateʼs thesis]. Moskovskii gosudarstvennii universitet. Moskva. [in Russian]

Bohdanova, M. I. (2001). Osoblyvosti vnutrishnoi budovy prynasuvnoi chastyny skyby Zelemianka. Visnyk Lvivskoho universytetu. Seriia heolohichna, 15, 144–151. [in Ukrainian]

Boyer, S. E., & Elliott, D. (1982). Thrust systems. Bulletin of the American Association of Petroleum Geologists, 66(9), 1196–1230. https://doi.org/10.1306/03B5A77D-16D1-11D7-8645000102C1865D

Festa, A., Pini, G. A., Ogata, K., & Dilek, Y. (2019). Diagnostic features and field-criteria in recognition of tectonic, sedimentary and diapiric mélanges in orogenic belts and exhumed subduction-accretion complexes. Gondwana Research, 74, 7–30. https://doi.org/10.1016/j.gr.2019.01.003

Fossen, H. (2016). Structural Geology (2nd ed.). Cambridge: Cambridge University Press. https://doi.org/10.1017/9781107415096

Hnylko, O. M. (2012). Tektonichne raionuvannia Karpat u svitli tereinovoi tektoniky. Stattia 2. Flishovi Karpaty – davnia akretsiina pryzma. Heodynamika, 1(12), 67–78. https://doi.org/10.23939/jgd2012.01.067 [in Ukrainian]

Kalinin, V. I., Hurskyi, D. S., & Antakova, I. V. (Eds.). (2006). Heolohichni pamiatky Ukrainy (Vol. 1). Kyiv: Derzhavna heolohichna sluzhba Ukrainy. [in Ukrainian]

Lukiienko, O. I., Vakarchuk, S. H., & Kravchenko, D. V. (2014). Strukturno-parahenetychnyi analiz (na tektonofatsialnii osnovi): Vol. 1. Epizona. Kyiv. [in Ukrainian]

McClay, K. R. (1992). Glossary of thrust tectonics terms. In K. R. McClay (Ed.), Thrust Tectonics (pp. 419–433). London: Chapman and Hall.

McClay, K. R., & Insley, M. W. (1986). Duplex structures in the Lewis thrust sheet, Crowsnest Pass, Rocky Mountains, Alberta, Canada. Journal of Structural Geology, 8(8), 911–922. https://doi.org/10.1016/0191-8141(86)90036-2

Schmid, S. M., Fügenschuh, B., Kounov, A., Maţenco, L., Nievergelt, P., Oberhänsli, R., Pleuger, J., Schefer, S., Schuster, R., Tomljenović, B., Ustaszewski, K., & van Hinsbergen, D. J. J. (2020). Tectonic units of the Alpine collision zone between Eastern Alps and western Turkey. Gondwana Research, 78, 308–374. https://doi.org/10.1016/j.gr.2019.07.005

Starzec, К., Malata, E., Wronka, A., & Malina, L. (2015). Mélanges and broken formations at the boundary zone of the Magura and Silesian nappes (Gorlice area, Polish Outer Carpathians) – a result of sedimentary and tectonic processes. Geological Quarterly, 59(1), 169–178. https://doi.org/10.7306/gq.1173

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AGE AND SEDIMENTARY ENVIRONMENTS OF THE PALEOCENE DEPOSITS IN THE CARPATHIAN SKYBA NAPPE BASED ON MICROPALEONTOLOGICAL AND SEDIMENTOLOGICAL DATA

Home > Archive > No. 1–2 (187–188) 2022 > 36–47

Geology & Geochemistry of Combustible Minerals No. 1–2 (187–188) 2022, 36–47.

https://doi.org/10.15407/ggcm2022.01-02.036

Oleh HNYLKO, Aida ANDREEVA-GRIGOROVICH, Svitlana HNYLKO

Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, Ukraine, e-mail: igggk@mail.lviv.ua

Abstract

The results of micropaleontological and sedimentological studies of the Paleocene sediments such as the Upper Member of the Stryi Formation and the Yamna Formation located in the Skyba Nappe in the Ukrainian Outer (Flysh) Carpathians are represented. Sedimentological features of the flysch successions (including the sedimentary succession along the Prut River in the city of Yaremche) proved that the Upper Member of the Stryi Formation is represented mainly by turbidites; the lower part of the Yamna Formation (variegated Yaremcha Horizon) is composed of red and green clay hemipelagites and turbidites, and the upper part of the Yamna Formation (Yamna sandstone) consists of deposits of high-density turbidite currents and grain flows.

The calcareous nannoplankton: NP1, NP2, NP3 and NP4 zones as well as the foraminifera: planktonic Globoconusa daubjergensis Zone (Danian Stage) and benthic Rzehakina epigona Subzone of Rzehakina fissistomata Zone, s. l. (the early Paleocene) are identified in the Upper Member of the Stryi Formation. The calcareous nannoplanktonic NP4, NP5, NP6 zones are distinguished in the Yaremcha Horizon and NP6, NP8, NP9 zones are identified in the Yamna sandstone. The agglutinated foraminifera including Rzehakina fissistomatа, Rz. epigona, Caudammina ovula, Hormosina velascoense, Glomospirella grzybowskii, Saccammina placenta, Paratrochamminoides irregularis are dominated in the Yamna Formation. The age of the Stryi Formation (Upper Member) is established as Danian–partly Zealandian, and the age of the Yamna Formation is Zealandian–Thanetian based on nannoplankton and foraminifera data.

Deep-water agglutinated foraminifera (DWAF) belonging to the genera Rhabdammina, Hyperammina, Dendrophrya, Ammodiscus, Glomospira, Hormosina, Reophax, Haplophragmoides, Recurvoides, Trochamminoides, Paratrochamminoides, Spiroplectammina, Karreriella are dominated in the background hemipelagic clay deposits and make up to 100% of the tests in the microfaunal associations, that suggests the lower bathyal-abyssal depths of the sedimentary paleobasin The channel deposits (Yamna sandstone) and interchannel sediments (Upper Member of the Stryi Formation) of the ancient deep-sea fan are identified in the Paleogene flysch.

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Keywords

Ukrainian Carpathians, Skyba Nappe, Paleocene, foraminifera, nannoplankton, sedimentation

Referenses

Andreeva-Grigorovich, A. S. (1991). Zonalnaya stratigrafiya paleogena yuga SSSR po fitoplanktonu (dinotsisti i nanoplankton) [Zonal stratigraphy of the Paleogene of the south of the USSR according to phytoplankton (dinocysts and nanoplankton)] [Extended abstract of Doctorʼs thesis]. Institut geologicheskikh nauk AN USSR. Kiev. [in Russian]

Andreeva-Grigorovich, A. S. (1994). Zonalnaya shkala po tsistam dinoflagellat dlya paleogena yuzhnikh regionov SNG [Zonal scale for dinoflagellate cysts for the Paleogene of the southern regions of the CIS]. Algologiya, 42, 66‒76. [in Russian]

Andreeva-Grigorovich, A. S., Vyalov, O. S., Gavura, S. P., Gruzman, A. D., Dabagyan, N. V., Danish, V. V., Ivanik, M. M., Kulchitskii, Ya. O., Lozinyak, P. Yu., Maslun, N. V., Petrashkevich, M. Y., Ponomareva, L. D., Portnyagina, L. A., Smirnov, S. Ye., & Sovchik, Ya. V. (1984). Obyasnitelnaya zapiska k regionalnoi stratigraficheskoi skheme paleogenovikh otlozhenii Ukrainskikh Karpat [Explanatory note to the regional stratigraphic scheme of the Paleogene deposits of the Ukrainian Carpathians] [Preprint N 84-19]. Kiev: Institut geologicheskikh nauk AN USSR. [in Russian]

Andreyeva-Grigorovich, A. S. (1999). Biostratigraphic correlations of the Paleogene deposits of the Ukrainian Carpathians and Crimea-Bakhchisarai area using nannoplankton and dinocysts. Geologica Carpathica, 50, 10–12.

Andrieieva-Hryhorovych, A., Maslun, N., Hnylko, S., & Hnylko, O. (2014). Pro vik i umovy sedymentatsii horyzontiv strokatykh arhilitiv u paleotsen-eotsenovykh vidkladakh Ukrainskykh Karpat [About the age and sedimentary conditions of variegated mudstone horizons in the Paleocene-Eocene deposits of the Ukrainian Carpathians]. In Materialy V Vseukrainskoi naukovoi konferentsii “Problemy heolohii fanerozoiu Ukrainy”: tezy dopovidei (pp. 3–6). Lviv: Lvivskyi natsionalnyi universytet imeni I. Franka. [in Ukrainian]

Einsele, G. (1992). Sedimentary Basins: evolution, facies and sediment budget. Berlin: Springer–Verlag. https://doi.org/10.1007/978-3-642-77055-5

Golonka, J., Gahagan, L., Krobicki, M., Marko, F., Oszczypko, N., & Ślączka, A. (2006). Plate tectonic evolution and paleogeography of the circum-Carpathian region. AAPG, Memoir, 84, 11–46. https://doi.org/10.1306/985606m843066

Golonka, J., Waśkowska, A., & Ślączka, A. (2019). The Western Outer Carpathians: Origin and evolution. Zeitschriftder Deutschen Gesellschaft für Geowissenschaften, 170(3–4), 229–254. https://doi.org/10.1127/zdgg/2019/0193

Hnylko, O. M. (2012). Tektonichne raionuvannia Karpat u svitli tereinovoi tektoniky. Stattia 2. Flishovi Karpaty – davnia akretsiina pryzma [Tectonic zoning of the Carpathians in term`s of the terrane tectonics, article 2. The Flysch Carpathian – ancient accretionary prism]. Heodynamika, 1(12), 67–78. https://doi.org/10.23939/jgd2012.01.067 [in Ukrainian]

Hnylko, O. (2016). Heolohichna budova ta evoliutsiia Ukrainskykh Karpat [Geological structure and evolution of the Ukrainian Carpathians] [Extended abstract of Doctorʼs thesis]. Lvivskyi natsionalnyi universytet imeni I. Franka. Lviv. [in Ukrainian]

Hnylko, O. M., & Slotiuk, B. M. (1993). Do heolohichnoi paleookeanohrafii pivnichno-zakhidnoi chastyny Ukrainskykh Karpat (basein verkhnoi techii r. Dnister). Rannia kreida–eotsen [To the geological paleoceanography of the northwestern part of the Ukrainian Carpathians (basin of the upper reaches of the Dnister River). Early Cretaceous–Eocene]. Heolohiia i heokhimiia horiuchykh kopalyn, 2–3(84–85), 80–86. [in Ukrainian]

Ivanik, M. M., & Maslun, N. V. (1977). Kremnistie mikroorganizmi i ikh ispolzovanie dlya raschleneniya paleogenovikh otlozhenii Predkarpatya [Siliceous microorganisms and their use for dismemberment of the Paleogene deposits of the Fore-Carpathians]. Kiev: Naukova dumka. [in Russian]

Kaminski, M. A., & Gradstein, F. M. (2005). Atlas of Paleogenecosmopolitan deep-water agglutinated foraminifera. Grzybowski Foundation Special Publication, 10.

Kováč, M., Márton, E., Oszczypko, N., Vojtko, R., Hók, J., Králiková, S., Plašienka, D., Klučiar, T., Hudáčková, N., & Oszczypko-Clowes, M. (2017). Neogene palaeogeography and basin evolution of the Western Carpathians, Northern Pannonian domain and adjoining areas. Global and Planetary Change, 155, 133–154. https://doi.org/10.1016/j.gloplacha.2017.07.004

Kováč, M., Plašienka, D., Soták, J., Vojtko, R., Oszczypko, N., Less, G., Ćosović, V., Fügenschuh, B., & Králiková, S. (2016). Paleogene palaeogeography and basin evolution of the Western Carpathians, Northern Pannonian domain and adjoining areas. Global and Planetary Change, 140, 9–27. https://doi.org/10.1016/j.gloplacha. 2016.03.007

Maslakova, N. I. (1955). Stratigrafiya i fauna melkikh foraminifer paleogenovikh otlozhenii Vostochnikh Karpat [Stratigraphy and fauna of small foraminifers in the Paleogene deposits of the Eastern Carpathians]. Moskva: Gosgeolizdat. [in Russian]

Matskiv, B. V., Pukach, B. D., & Hnylko, O. M. (2009). Derzhavna heolohichna karta Ukrainy masshtabu 1 : 200 000. Arkushi M-35-XXXI (Nadvirna), L-35-I (Visheu-De-Sus). Karpatska seriia. Heolohichna karta dochetvertynnykh utvoren [State geological map of Ukraine on a scale of 1:200,000. Sheets M-35-XXXI (Nadvirna), L-35-I (Visheu-De-Sous). Carpathian series. Geological map of pre-Quaternary formations]. Kyiv: UkrDHRI. [in Ukrainian]

Pilipchuk, A. S. (1972). Litologicheskie osobennosti i usloviya obrazovaniya pestrotsvetnikh otlozhenii Skibovoi zoni Karpat [Lithological features and conditions for the formation of the variegated deposits in the Skyba Zone of the Carpathians]. In Novie dannie po geologii i neftegazonosnosti USSR (pp. 101–110). Lvov: Izdatelstvo Lvovskogo universiteta. [in Russian]

Reding, Kh. G., Kollinson, Dzh. D., Allen, F. A., Elliott, T., Shreiber, B. Sh., Dzhonson, G. D., Bolduin, K. T., Sellvud, B. U., Dzhenkins, X. K., Stou, D. A. V., Eduardz, M., & Mitchell, A. X. G. (1990). Obstanovki osadkonakopleniya i fatsii [Sedimentary environments and facies] (Kh. Reding, Ed.; B. V. Baranov, I. S. Barskov, L. N. Indolev, M. A. Levitan & I. O. Murdmaa, Trans.; Vol. 2). Moskva: Mir. [in Russian]

Schmid, S., Bernoulli, D., Fugenschuh, B., Matenco, L., Schefer, S., Schuster, R., Tischler, M., & Ustaszewski, K. (2008). The Alpine-Carpathian-Dinaric orogenic system: correlation and evolution of tectonic units. Swiss Journal of Geosciences, 101, 139–183. https://doi.org/10.1007/s00015-008-1247-3

Senkovskyi, Yu., Hryhorchuk, K., Hnidets, V., & Koltun, Yu. (2004). Heolohichna paleookeanohrafiia okeanu Tetis [Geological paleoceanography of the Tethys Ocean]. Kyiv: Naukova dumka. [in Ukrainian]

Vyalov, O. S. (1951). Skhema stratigrafii severnogo sklona Karpat [Stratigraphy scheme of the northern slope of the Carpathians]. Dokladi Akademii nauk SSSR, 7(77), 689–692. [in Russian]

Vyalov, O. S., Gavura, S. P., Danish, V. V., Lemishko, O. D., Leshchukh, R. Y., Ponomareva, L. D., Romaniv, A. M., Smirnov, S. Ye., Smolinskaya, N. I., & Tsarnenko, P. N. (1988). Stratotipi melovikh i paleogenovikh otlozhenii Ukrainskikh Karpat [Stratotypes of the Cretaceous and Paleogene deposits of the Ukrainian Carpathians]. Kiev: Naukova dumka. [in Russian]

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GEOLOGICAL GROUNDS OF PERSPECTIVE ZONES FOR THE ACCUMULATION OF BEHIND-PIPE GAS RESERVES (East-Novoselovskyi Oil-Gas Condensate Field, Dnieper-Donets Depression)

Home > Archive > No. 1–2 (187–188) 2022 > 27–35

Geology & Geochemistry of Combustible Minerals No. 1–2 (187–188) 2022, 27–35.

https://doi.org/10.15407/ggcm2022.01-02.027

Vyacheslav LUKINOV1, Kostyantyn BEZRUCHKO1, Oleksii PRYKHODCHENKO1, Vladyslav KOBEZA2

1 M. S. Polyakov Institute of Geotechnical Mechanics of National Academy of Sciences of Ukraine, Dnipro, Ukraine, e-mail: gvrvg@meta.ua
2 “Shebelinkagazvydobuvannia” Gas Industry Department of Ukrgazvydobuvannia JSC, Donets, Kharkiv Region, Ukraine, e-mail: Kobeza15@gmail.com

Abstract

The practical experience of long-term operation of hydrocarbon deposits confirms the presence of geomechanical processes and their significant impact on the state of the gas-saturated massif of rocks. In fields that are being operated for a long time, the prospects for industrial hydrocarbon accumulation can be associated with secondary gas traps of non-traditional type, in particular, technogenic ones, which are formed in low-pore reservoirs. A detailed analysis of the geological conditions of the East-Novoselovskyi field was carried out. They contribute to the formation of additional gas resources (“behind-pipe reserves” category), as well as the establishment of geological-industrial indices of the perspectivity for the formation of technogenic deposits was carried out.

The purpose of the work is geological justification and finding perspective zones for the accumulation of behind-pipe reserves through the formation of technogenic deposits under the impact of a geomechanical factor, using the example of the East-Novoselovskyi oil-gas condensate field.

For the geological conditions of the East-Novoselovskiy Oil-Gas Condensate Field, producing the additional gas reserves should be expected from technogenic deposits that are located above the industrial horizons that are being developed and formed in low-porous reservoirs under the action of a geomechanical factor, as a result of their decompaction after gas extraction from an industrial reservoir as a result of its compression. In accordance with the conducted research, the most perspective section, from the standpoint of the formation of a technogenic deposit and the accumulation of behind-pipe reserves, within the East-Novoselovskyi Oil-Gas Condensate Field there is the strata identified in the area of wells No. 16, 18, 60, in the section interval at a distance of 92.4 m up from the roof of the horizon (B-3b), which is located from a depth of 2141 m to the roof of the horizon B-3a, at a depth of 2 233 m. It is worthwhile to further carry out appropriate geophysical work for conducting the technological work for the development of technogenic deposits in perspective zones behind the casing column in operated wells.

The account of the geomechanical factor opens up the perspective of producing the additional industrial gas influx at the late stages of the development of gas and gas-condensate fields, by predicting the geological conditions for the formation of the improved secondary filtration-capacitive properties favorable to form technogenic gas deposits.

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Keywords

gas fields, geomechanical factor, technogenic reservoir, behind-pipe reserves

Referenses

Abielientsev, V. M., Lurie, A. Y., Povieriennyi, S. F., & Susiak, T. Ya. (2017). Nova metodyka interpretatsii rezultativ laboratornykh doslidzhen hirskykh porid pry modeliuvanni plastovykh umov [A new method for interpreting the results of laboratory studies of rocks in modeling reservoir conditions]. Heolohichnyi zhurnal, 3, 23–30. https://doi.org/10.30836/igs.1025-6814.2017.3.117319 [in Ukrainian]

Bulat, A. F., Lukinov, V. V, Bezruchko, K. A., Krukovskyi, O. P., & Krukovska, V. V. (2018). Heomekhanichnyi chynnyk nadkhodzhennia dodatkovykh obsiahiv vilnoho metanu pry ekspluatatsii hazovykh rodovyshch [Geomechanical factor of receipt of additional volumes of free methane during the operation of gas fields]. Dopovidi Natsionalnoi akademii nauk Ukrainy, 8, 25–35. https://doi.org/10.15407/dopovidi2018.08.025 [in Ukrainian]

Bulat, A. F., Lukinov, V. V, Bezruchko, K. A., & Prykhodchenko, O. V. (2020). Vplyv heomekhanichnykh protsesiv na plastovyi tysk pry tryvalii ekspluatatsii hazovykh rodovyshch [Influence of geomechanical processes on reservoir pressure during long-term operation of gas fields]. Rozvidka ta rozrobka naftovykh ta hazovykh rodovyshch, 4(77), 62–76. https://doi.org/10.31471/1993-9973-2020-4(77)-62-76 [in Ukrainian]

Cheban, O. V., & Vladyka, V. M. (2007). Perspektyvy naroshchuvannia vydobutku hazu na starykh rodovyshchakh Peredkarpattia na prykladi Rudkivskoho hazovoho rodovyshcha [Prospects for increasing gas production at Old fields in the Carpathian region on the example of the Rudkovsky gas field]. Problemy naftohazovoi promyslovosti, 5, 326–328. [in Ukrainian]

Ivaniuta, M. M. (Ed.). (1998). Atlas rodovyshch nafty i hazu Ukrainy [Atlas of oil and gas fields in Ukraine] (Vol. 3. Ckhidnyi naftohazonosnyi rehion [Eastern oil and gas region]; Vol. 4. Zakhidnyi naftohazonosnyi rehion [Western oil and gas region]). Lviv: Ukrainska naftohazova akademiia. [in Ukrainian]

Klasyfikatsiia zapasiv i resursiv korysnykh kopalyn derzhavnoho fondu nadr [Classification of Mineral Reserves and resources of the state subsurface fund. (1997). Resolution of the Cabinet of Ministers of Ukraine  № 432. https://zakon.rada.gov.ua/laws/show/432-97-p#Text [in Ukrainian]

Kyryliuk, O. V., & Rudko, H. I. (Eds.). (2019). Nadrokorystuvannia v Ukraini [Subsurface use in Ukraine]. Chernivtsi: Bukrek. [in Ukrainian]

Lukinov, V. V., Bezruchko, K. A., Prykhodchenko, O. V., & Kobeza, V. S. (2021). Pokaznyky perspektyvnosti otrymannia dodatkovykh pryplyviv vuhlevodniv na hazovykh rodovyshchakh [Indicators of prospects for obtaining additional hydrocarbon inflows in gas fields]. In Vid Mineralohii i Heohnozii do Heokhimii, Petrolohii, Heolohii ta Heofizyky: fundamentalni i prykladni trendy XXI stolittia [From Mineralogy and Geognosia to geochemistry, Petrology, Geology and Geophysics: fundamental and applied trends of the XXI century]: materialy konferentsii Kyivskoho natsionalnoho universytetu imeni T. H. Shevchenka (Kyiv, Ukraina, 28–30 veresnia 2021 r.) (pp. 193–197). Kyiv. [in Ukrainian]

Lukinov, V. V., Prykhodchenko, V. F., Zhykaliak, M. V., & Prykhodchenko, O. V. (2016). Metody prohnozu hirnycho-heolohichnykh umov rozrobky vuhilnykh rodovyshch [Methods for predicting mining and geological conditions for coal field development]. Dnipro: NHU. [in Ukrainian]

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TECTONIC UNITS OF THE KROSNO (SILESIA) COVER OF THE FOLDED CARPATHIANS: TYKHIY (UKRAINE) AND VETLINA (POLAND) STRUCTURES – GEOLOGICAL STRUCTURE AND GAS-BEARING POTENTIAL

Home > Archive > No. 1–2 (187–188) 2022 > 5–26

Geology & Geochemistry of Combustible Minerals No. 1–2 (187–188) 2022, 5–26.

https://doi.org/10.15407/ggcm2022.01-02.005

Myroslav PAVLYUK, Volodymyr SHLAPINSKY, Myroslav TERNAVSKY

Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, Ukraine, e-mail: igggk@mail.lviv.ua

Abstract

In the south-western part of the Krosno cover in the terrain of the Ukraine, that is called jednostka Szląska (Silesia Unit) in the adjoining Polish territory, two tectonic structures Tykhiy and Vetlina composed of flysh of the Cretaceous-Paleogene age, are correspondingly present. They are in the same scale and represent preserved anticlinal fold of the north-western strike. The Tykhiy and Vetlina structures were defined according to results of drilling. In consequence of executed drilling works the commercial gas presence of both structures was determined. Maximum gas discharges from the deposits of Oligocene at both structures are estimated to be approximately 60th m3/day. The production reserves of the Vetlina structure are estimated at 73 million m3 of gas. The deposit is not being developed due to localization in the area within the Beskydy National Park. The authors don’t recommend to carry out exploratory drilling within the limits of the structure, in located further north-east of the Tykhiy structure the Volosianka–Pidpolozzia and Husne–Bukovets scales as the ineffective drilling because of the absence of perspective objects in their composition. There are prerequisites to suppose the presence of just one more gas-saturated fold, Liuta, further south-west of the Tykhiy structure, under the Duklya–Chornohora cover. It is located within the hydrocarbon field, favourable for the search for hydrocarbons. The potential industrial gas potential of the forecasted promising structure is evidenced by the inflows of oil and gas in the mapping wells of Liuta Square. Significant manifestations of hydrocarbons were observed in well 18-Liuta. From a depth of 40 m, and then 190 m recorded oil manifestations – oil films on the surface of the clay solution (d 20 – 0.843 g/cm3; viscosity in 0E – 1.92; S – 0.22 %, the beginning of boiling – 97 °C, up to 350 °C – 56 %). Intense gas manifestations were noted from a depth of 167 m (CH4 – 95.36 %; CO2 – 1.01 %; N2 – 3.63 %). To check this supposition, it is expedient to conduct seismic survey.

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Keywords

Krosno cover, Tykhiy and Vetlina structures, geological structure, gas-bearingness

Referenses

Hlushko, V. V., Kuzovenko, V. V., & Shlapinskyi, V. Ye. (1999). Novi pohliady na heolohichnu budovu pivnichno-zakhidnoi chastyny Duklianskoho pokrovu Ukrainskykh Karpat. Visnyk Lvivskoho universytetu. Seriia heolohichna, 13, 94–101. [in Ukrainian]

Karnkowski, P. (1993). Złoża gazu ziemnego i ropy naftowej w Polsce: T. 2. Karpaty i zapadlisko Przedkarpackie. Częśc 1. Karpaty. Kraków.

Komunikat rządu Rzeczypospolitej Polskiej dotyczący dyrektywy 94/22/WE Parlamentu Europejskiego i Rady w sprawie warunków udzielania i korzystania z zezwoleń na poszukiwanie, badanie i produkcję węglowodorów. (2019). https://www.prawo.pl/akty/dz-u-ue-c-2019-105-76,69161005.html

Kowalczyk, A. (12.01.2012). Aurelian z dwiema nowymi koncesjami. Rynek Infrastruktury. https://www.rynekinfrastruktury.pl/wiadomosci/aurelian-z-dwiema-nowymi-koncesjami-36271.html

Krupskyi, Yu. Z., Kurovets, I. M., Senkovskyi, Yu. M., Mykhailov, V. A., Chepil, P. M., Dryhant, D. M., Shlapinskyi, V. Ye., Koltun, Yu. V.,Chepil, V. P., Kurovets, S. S., & Bodlak, V. P. (2014). Netradytsiini dzherela vuhlevodniv Ukrainy: Vol. 2. Zakhidnyi naftohazonosnyi rehion. Kyiv: Nika-Tsentr. [in Ukrainian]

Kuzovenko, V. V., Zhigunova, Z. F., & Petrov, V. G. (1973). Otchet o rezultatakh kompleksnoi geologicheskoi syomki masshtaba 1 : 50 000, provedennoi na ploshchadi Lomna Lvovskoi i Zakarpatskoi oblastei USSR v 1969–1972 gg. Trest “Lvovneftegazrazvedka”, KGP. Lvov: Fondy DP “Zakhidukrheolohiia”. [in Russian]

Marcińkowski, A., & Szewczyk, E. (2008). Produktywność karpackich skal zbiórnikowych w świetle historii wydobycia więglowodorów. Geologia, 34(3), 405–421.

Mochalin, I. P., & Nekrasova, L. P. (1964). Otchet o geologicheskikh issledovaniyakh, provedennikh na ploshchadi Lugi Zakarpatskoi oblasti USSR v 1963 g. Lvov: Fondy DP “Zakhidukrheolohiia”. [in Russian]

Shlapinskyi, V. Ye., Hlushko, V. V., & Kuzovenko, V. V. (1994). Vyvchennia heolohichnoi budovy i perspektyv naftohazonosnosti zony zchlenuvannia Duklianskoho, Chornohorskoho i Krosnenskoho pokroviv Ukrainskykh Karpat v 1991–1994 rr. (Vol. 1). Lviv: Fondy DP “Zakhidukrheolohiia”. [in Ukrainian]

Szuflicki, M., Malon, A., & Tymiński, M. (Eds.). (2021). Bilans zasobów złóż kopalin w Polsce wg stanu na 31 XII 2020 r. Warszawa: Państwowy Instytut Geologiczny–Państwowy Instytut Badawczy. Publikacja dostępna na stronie internetowej http://surowce.pgi.gov.pl

Vyalov, O. S., Gavura, S. P., Danish, V. V., Lemishko, O. D., Leshchukh, R. Y., Ponomareva, L. D., Romaniv, A. M., Smirnov, S. Ye., Smolinskaya, N. I., & Tsarnenko, P. N. (1988). Stratotipi melovikh i paleogenovikh otlozhenii Ukrainskikh Karpat. Kiev: Naukova dumka. [in Russian]

Zhigunova, Z. F., Koval, Zh. S., & Petrov, V. G. (1966). Otchet o poiskovo-semochnikh rabotakh masshtaba 1 : 25 000, provedennikh na ploshchadi Lyuta Zakarpatskoi oblasti USSR v 1964–1965 gg. Trest “Lvovneftegazrazvedka”, LGPK. Lvov: Fondi DP “Zakhіdukrgeologіya”. [in Russian]

Zhigunova, Z. F., Petrov, V. G., & Tatarchenko, V. M. (1964). Otchet o geologicheskikh issledovaniyakh, provedennikh na ploshchadi Bukovets Zakarpatskoi oblasti USSR v 1963 godu. Trest “Lvovneftegazrazvedka”, LGPK. Lvov: Fondi DP “Zakhіdukrgeologіya”. [in Russian]

Zielińska, Cz. (1994). Dokumentacja geologiczna w kat. C złoża gazu ziemnego “Wetlina” w miejsc. Smerek i Wetlina, gm. Cisna, woj. krośnińskie. Nr CBDG 85621. Inw. 1481/95 Arch. CAG PIG, Warszawa; Kat. DZ/418 Arch. PGNiG S.A., Warszawa. http://dokumenty.pgi.gov.pl/wyszukiwarka/dokument/85621?lang=pl

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SUBSTANDARD COMBUSTIBLE MINERALS OF UKRAINE AND PRINCIPLES OF THEIR ECOLOGICAL CONVERSION

Home > Archive > No. 1–2 (187–188) 2022 > 127–140

Geology & Geochemistry of Combustible Minerals No. 1–2 (187–188) 2022, 127–140.

https://doi.org/10.15407/ggcm2022.01-02.127

Dmytro BRYK, Myroslav PODOLSKY, Lesia KULCHYTSKA-ZHYHAILO, Oleh GVOZDEVYCH

Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, Ukraine, e-mail: cencon@ukr.net

Abstract

In the general case, substandard combustible minerals include on-balance and off-balance reserves of primary energy materials – coal and peat deposits (solid combustible minerals) and oil and natural gas deposits (liquid and gaseous combustible minerals), which by physico-chemical, energy or geological-spatial conditions do not meet the economic criteria for extraction and use of traditional technological methods, as well as the potential of methane from coal deposits, arrays of man-made carbon-containing materials such as waste from coal mining, coal beneficiation, refining, etc. Review of the available reserves in terms of the use of modern technologies of environmentally friendly conversion can significantly expand the opportunities for the development of all types of combustible minerals in Ukraine.

The paper considers the geological zoning of oil and gas fields and deposits of solid combustible minerals, as well as their reserves and production. It is shown that the reserves of the main primary energy resources in Ukraine many times exceeds the extraction and has significant opportunities to increase due to the use of substandard combustible minerals.

The principles of ecologically safe conversion of substandard combustible minerals in terrestrial and underground conditions are presented. The importance of energy utilization of methane from coal deposits, arrays of such man-made carbon-containing materials as coal mining waste, coal beneficiation, oil refining, etc. was noted. The main mining-geological and technological criteria that contribute to the development of coal seams by underground gasification are given, as well as deposits and areas of coal basins of Ukraine that are suitable for underground gasification.

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Keywords

combustible minerals, coal, gasification, ecological conversion

Referenses

Bryk, D., Hvozdevych, O., Kulchytska-Zhyhailo, L., & Podolskyi, M. (2019). Tekhnohenni vuhlevmisni obiekty Chervonohradskoho hirnychopromyslovoho raionu ta deiaki tekhnichni rishennia yikhnoho vykorystannia. Heolohiia i heokhimiia horiuchykh kopalyn, 4(181), 45–65. https://doi.org/10.15407/ggcm2019.04.045 [in Ukrainian]

Bryk, D. V., Podolskyi, M. R., & Hvozdevych, O. V. (2014). Fizyko-tekhnichne obgruntuvannia vyrobnytstva syntetychnoho palyva z vuhillia (na prykladi Lvivsko-Volynskoho baseinu). Uglekhimicheskii zhurnal, 4, 69–74. [in Ukrainian]

Bryk, D., Podolskyi, M., Khokha, Yu., Liubchak, O., Kulchytska-Zhyhailo, L., & Hvozdevych, O. (2021). Nekondytsiini vuhletsevmisni horiuchi kopalyny ta sposoby yikhnoho termokhimichnoho pereroblennia. Heolohiia i heokhimiia horiuchykh kopalyn, 1–2(183–184), 89–109. https://doi.org/10.15407/ggcm2021.01-02.089 [in Ukrainian]

Derzhavna sluzhba statystyky Ukrainy. (2020). Palyvno-enerhetychni resursy Ukrainy. Statystychnyi zbirnyk. https://ukrstat.gov.ua/druk/publicat/kat_u/2020/zb/12/Zb_per.pdf [in Ukrainian]

DHP “Zakhidukrheolohiia”, VO “Volynvuhillia”, DKhH “Lvivvuhillia” (2002). Heoloho-promyslova karta Lvivsko-Volynskoho kamianovuhilnoho baseinu. [in Ukrainian]

Falbe, Yu. M. (1980). Khimicheskie veshchestva iz uglya. Moskva: Khimiya. [in Russian]

“Heoinform Ukrainy”. (2020). http://minerals-ua.info/mapviewer/goruchi.php [in Ukrainian]

Ivantsiv, O. Ye., Kukhar, Z. Ya., & Bryk, D. V. (2001). Novi pidkhody do perspektyv pidzemnoi hazyfikatsii vuhilnykh rodovyshch Ukrainy. Heolohiia i heokhimiia horiuchykh kopalyn, 2, 129–134. [in Ukrainian]

Kurovets, I. M., Mykhailov, V. A., Zeikan, O. Yu., Krupskyi, Yu. Z., Hladun, V. V., Chepil, P. M., Hulii, V. M., Kurovets, S. S., Kasianchuk, S. V., Hrytsyk, I. I., & Naumko, I. M. (2014). Netradytsiini dzherela vuhlevodniv Ukrainy: Vol. 1. Netradytsiini dzherela vuhlevodniv: ohliad problemy. Kyiv: Nika-tsentr. [in Ukrainian]

Maistrenko, A. Yu., Dudnik, A. N., & Yatskevich, S. V. (1998). Tekhnologii gazifikatsii uglei dlya parogazovikh ustanovok. Kiev: Znanie. [in Russian]

Podolskyi, M., Bryk, D., Kulchytska-Zhyhailo, L., & Hvozdevych, O. (2021). Vykorystannia horiuchykh kopalyn u konteksti tsilei staloho rozvytku Ukrainy ta hlobalnykh zmin navkolyshnoho seredovyshcha. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4(185–186), 109–125. https://doi.org/10.15407/ggcm2021.03-04.109 [in Ukrainian]

Savchak, O. (2019). Heoloho-heokhimichni osoblyvosti mihratsii ta formuvannia hazovykh rodovyshch u naftohazonosnykh rehionakh Ukrainy. Heolohiia i heokhimiia horiuchykh kopalyn, 1(178), 21–40. https://doi.org/10.15407/ggcm2019.01.021 [in Ukrainian]

Stefanik, Yu. V. (1990). Geotekhnologiya nekonditsionnikh tverdikh topliv. Kiev: Naukova dumka. [in Russian]

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GEOLOGICAL STRUCTURE AND PROSPECTS OF OIL-GAS PRESENCE AT THE POHAR PLOT (Folded Carpathians)

Home > Archive > No. 3–4 (185–186) 2021 > 5–15

Geology & Geochemistry of Combustible Minerals No. 3–4 (185–186) 2021, 5–15.

https://doi.org/10.15407/ggcm2021.03-04.005

Volodymyr SHLAPINSKY, Myroslav PAVLYUK, Yaroslav LAZARUK, Olesya SAVCHAK, Myroslav TERNAVSKY

Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, Ukraine, e-mail: vlash.ukr@gmail.com

Abstract

The Pohar plot is situated in the Skole district of the Lviv Region, 30 km south-west of Skole town, between Pohar and Kryve villages. Tectonically it is located in of junction of the Skybian (Slavske Skyba) and the Krosno covers. At the end of XIX beginning of XX centuries in the region of the village the oil-extracting enterprise was existent. There deposits of Oligocen and Eocene of the Rozluch belt of the Krosno cover and Oligocene of the scale of the Slavske skyba of the Skybian cover were exploited. During two ten-years of exploitation by exploring shafts and shallow boreholes more than 3 thousand ton of oil was extracted. Prospects of the Pohar plot should be connected with sand horizons of the Holovets suite of Oligocen (Klivsky sandstones) that are characterized by satisfactory reservoir properties. They are localized in the immersed part of the Hrosivsky scale of the Krosno cover separated by the Rozluch fault (tectonically screened deposit) from its forkball part, drilled in 1973–1974 1-Pohar borehole (well bottom 1935 m), due to deflection of its hole to the south-east, didn’t expose the Klivsky sandstones and didn’t solve its task. For complete exposition of the Klivsky sandstones of the Holovets suite of Oligocene of the Hrosivsky scale it is necessary to design vertically oriented 2-Pohar borehole of 2300 m in depth. About probable commercial oil-gas saturation of the horizon of the Klivsky sandstones testifies not only to the existence of the oil-extracting enterprise in the past, but the intensive surface oil shows in the stretched area that is controlled by the Rozluch fault. Moreover, taking the prospect of the zone of junction of the given covers in consideration, the seismic survey should be conducted at the Pohar area for the estimation of the geological structure of the deeper horizons and parametric borehole of 4000–5000 m in depth should be designed.

Full Text

Keywords

Skybian and Krosno covers, Rozluch fault, oil extracting enterprise, prospects of oil-gas presence

Referenses

Kantolinskii, S. I., & Nekrasova, L. P. (1975). Geologicheskii otchet o rezul’tatakh strukturno-poiskovogo bureniya, provedennogo na ploshchadi Pogar L’vovskoi oblasti USSR v 1973–1974 gg. Trest “L’vovneftegazrazvedka”, KGP. L’vov: Fondy DP “Zakhidukrheolohiia”. [in Russian]

Kuzovenko, V. V., Glushko, V. V., Myshkin, L. P., & Shlapinskii, V. E. (1990). Izuchenie geologo-geofizicheskikh materialov po Skibovoi i Krosnenskoi zonam Skladchatykh Karpat, s tsel’yu vyyavleniya perspektivnykh na neft’ i gaz ob”ektov za 1988–1990 gg. PGO “Zapadukrgeologiya”. L’vov: Fondy DP “Zakhidukrheolohiia”. [in Russian]

Kuzovenko, V. V., Zhigunova, Z. F., & Petrov, V. G. (1977). Otchet o rezul’tatakh gruppovoi kompleksnoi geologicheskoi s”emki masshtaba 1 : 50 000, provedennoi na ploshchadi Klimets L’vovskoi i Zakarpatskoi oblastei USSR v 1973–1976 gg. Trest “L’vovneftegazrazvedka”, KGP. L’vov: Fondy DP “Zakhidukrheolohiia”. [in Russian]

Kyk, I. V., Chizh, E. I., & Ratych, V. A. (1966). Otchet o rezul’tatakh profil’nogo strukturno-poiskovogo bureniya na ploshchadi Turka L’vovskoi oblasti USSR, provedennogo v 1964–1965 gg. L’vov: Fondy DP “Zakhidukrheolohiia”. [in Russian]

Shlapinskyi, V. Ye., Havryshkiv, H. Ya., & Haievska, Yu. P. (2020). Kolektory nafty i hazu v kreidovo-paleotsenovykh vidkladakh Skybovoho pokryvu Ukrainskykh Karpat (pivnichno-zakhidna i tsentralna dilianky) ta perspektyvy yikh naftohazonosnosti. Heolohichnyi zhurnal, 3, 47–64. https://doi.org/10.30836/igs.1025-6814.2020.3.207341 [in Ukrainian]

Temnyuk, F. P. (1952). Otchet o geologicheskikh issledovaniyakh zony Krosno, provedennykh na ploshchadi Il’nik–Komarniki Drogobychskoi oblasti v 1951 g. L’vov: Fondy DP “Zakhidukrheolohiia”. [in Russian]

Wyszyński, O. W., & Obtułowicz, J. (1939). Antyklina Poharu. Budowa geologiczna i złoża ropy. Przemysł naftowy, 3, 65–68.

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СONSUMPTION OF COMBUSTIBLE MINERALS IN THE CONTEXT OF THE TARGETS OF SUSTAINABLE DEVELOPMENT OF UKRAINE AND GLOBAL ENVIRONMENT CHANGES

Home > Archive > No. 3–4 (185–186) 2021 > 109–125

Geology & Geochemistry of Combustible Minerals No. 3–4 (185–186) 2021, 109–125.

https://doi.org/10.15407/ggcm2021.03-04.109

Myroslav PODOLSKYY, Dmytro BRYK, Lesia KULCHYTSKA-ZYHAILO, Oleh GVOZDEVYCH

Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, Ukraine, e-mail: cencon@ukr.net

Abstract

An analysis of Ukraine’s sustainable development targets, in particular in the field of energy, resource management and environmental protection, are presented. It is shown that regional energetic is a determining factor for achieving the aims of sustainable development.

Changes in the natural environment in Ukraine due to external (global) and internal (local) factors that are intertwined and overlapped can cause threats to socio-economic development. It is proved that in the areas of mining and industrial activity a multiple increase in emissions of pollutants into the environment are observed.

The comparison confirmed the overall compliance of the structure of consumption of primary energy resources (solid fossil fuels, natural gas, nuclear fuel, oil and petroleum products, renewable energy sources) in Ukraine and in the European Union, shows a steaby trend to reduce the share of solid fuels and natural gas and increasing the shares of energy from renewable sources.

For example, in Ukraine the shares in the production and cost of electricity in 2018 was: the nuclear power plants – 54.33 % and in the cost – 26.60 %, the thermal power – 35.95 and 59.52 %, the renewable energy sources – 9.6 and 13.88 %.

The energy component must be given priority, as it is crucial for achieving of all other goals of sustainable development and harmonization of socio-economic progress.

The paper systematizes the indicators of regional energy efficiency and proposes a dynamic model for the transition to sustainable energy development of the region.

Full Text

Keywords

combustible minerals, goals of sustainable development, ecology, energy efficiency indicators

Referenses

Barannik, V. O. (2017). Enerhoefektyvnist rehioniv Ukrainy: problemy otsinky ta naiavnyi stan. Dnipro: Instytut stratehichnykh doslidzhen, Rehionalnyi filial u m. Dnipro. [in Ukrainian]

Derzhavna sluzhba statystyky Ukrainy. Enerhetychnyi balans Ukrainy za 2017 rik. http://www.ukrstat.gov.ua/operativ/operativ2012/energ/en_bal/arh_2012.htm [in Ukrainian]

Dosvid krain Yevrosoiuzu z pidvyshchennia enerhoefektyvnosti, enerhoaudytu ta enerhomenedzhmentu z enerhooshchadnosti v ekonomitsi krain. (2017).  Kyiv: DP “NEK Ukrenerho”. http://energy.esco.agency/rubriki-zhurnala/jenergomenedzhment-v-jenergetike/4764/dosvid-krain-ievrosojuzu-z-pidvishhennja-energoefektivnosti-energoauditu-ta-energomenedzhmentu-z-energooshhadnosti-v-ekonomici-krain [in Ukrainian]

Eurostat. (2019). Energy balance sheets – 2017 data: 2019 edition. https://doi.org/10.2785/10223

Holovne upravlinnia statystyky u Lvivskii oblasti. (2019). http://database.ukrcensus.gov.ua/statbank_lviv/Database/24PRYRODA/databasetree_uk.asp [in Ukrainian]

Libanova, E. M., & Khvesyk, M. A. (Eds.). (2017). Sotsialno-ekonomichnyi potentsial staloho rozvytku Ukrainy ta yii rehioniv: vektory realnoho postupu: natsionalna dopovid. Kyiv: DU IEPSR NAN Ukrainy. [in Ukrainian]

Lvivenerhozbut. (2019). Taryfy. http://lez.com.ua/tariff/ [in Ukrainian]

Ministerstvo ekonomichnoho rozvytku i torhivli Ukrainy. (2017). Tsili staloho rozvytku: Ukraina. Natsionalna dopovid 2017. https://me.gov.ua/Documents/List?lang=uk-UA&id=938d9df1-5e8d-48cc-a007-be5bc60123b8&tag=TSiliStalogoRozvitku [in Ukrainian]

Ministerstvo ekonomiky Ukrainy. (2020). Dobrovilnyi natsionalnyi ohliad shchodo Tsilei staloho rozvytku v Ukraini. https://me.gov.ua/Documents/Detail?lang=uk-UA&id=a0fc2a99-ada3-4a6d-b65b-cb542c3d5b77&title=DobrovilniiNatsionalniiOgliadSchodoTsileiStalogoRozvitkuVUkraini [in Ukrainian]

Ministerstvo zakhystu dovkillia i pryrodnykh resursiv Ukrainy. (2020). Misiia ta stratehiia. https://mepr.gov.ua/content/misiya-ta-strategiya.html [in Ukrainian]

Navkolyshnie seredovyshche. (2012). In KOMPAS: Posibnyk z osvity v haluzi prav liudyny za uchasti molodi. https://www.coe.int/uk/web/compass/environment [in Ukrainian]

Podolskyi, M., & Bryk, D. (2020). Naukovi pidkhody dlia dosiahnennia tsilei staloho rozvytku Ukrainy. Zbirnyk naukovykh prats ΛΌГOΣ, 52–55. https://doi.org/10.36074/20.11.2020.v5.15  [in Ukrainian]

Podolskyi, M., Kulchytska-Zhyhailo, L., & Hvozdevych, O. (2020a). Pokaznyky enerhoefektyvnosti v konteksti tsilei staloho rozvytku Ukrainy. Materialy konferentsii MTsND, 27–31. https://doi.org/10.36074/02.10.2020.v1.05 [in Ukrainian]

Podolskyi, M., Kulchytska-Zhyhailo, L., & Hvozdevych, O. (2020b). Struktura ta tekhnolohichni aspekty vykorystannia enerhetychnykh resursiv v krainakh Yevropeiskoho Soiuzu ta v Ukraini. Zbirnyk naukovykh prats ΛΌГOΣ, 52–55. https://doi.org/10.36074/09.10.2020.v2.14 [in Ukrainian]