Tag: hydrocarbons

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PROSPECTS OF THE OIL AND GAS POTENTIAL OF THE NORTHERN YAVORIV AREA OF THE BILCHE-VOLYTSIA AREA OF THE FORECARPATHIAN (according to the results of comprehensive geophysical and geochemical research)

Home > Archive > No. 1–2 (193–194) 2024 > 69–80

Geology & Geochemistry of Combustible Minerals No. 1–2 (193–194) 2024, 69–80

https://doi.org/10.15407/ggcm2024.193-194.069

Stepan DUCHUK1, Sofiia MAKSYMUK2, Anatoliy GALAMAY3


1 Western-Ukrainian Geophysical Exploration Expedition, Lviv, Ukraine, e-mail: zugre@lviv.farlep.netInstitute of 2, 3 Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, Ukraine, e-mail: 2 danaarsen@ukr.net; 3 galamaytolik@ukr.net

Abstract

A complex of geophysical and geochemical studies was carried out in the Bilche-Volytsia zone on the Northern Yavoriv area with the aim of detailing the geological structure of Mesozoic and Neogene deposits in the context of identifying oil and gas promising traps of various types and preparing them for deep drilling.

To solve the problem, the following studies were applied: seismic surveying by the common depth point method, electrical surveying by the method of sounding the formation of the field in the near zone, geochemical surveying by the method of gas discharge surveying.

The main resulting material of the performed geophysical and geochemical studies on the Northern Yavoriv area is a structural-tectonic model, seismic and seismogeological sections, maps of longitudinal resistances and geoelectrical sections, maps of geochemical parameters, mapping maps by types of research.

As a result of conducting seismic, electrical, and geochemical studies, the geological structure of the Northern Yavoriv area was detailed. Structural plans by stratigraphic levels are presented: Pre-Neogene surface, Tyrassian of the Badenian age suite, the top of the Lower Dashava subsuite of Sarmatian age, the top of Upper Dashava subsuites of Sarmatian age.

The Pre-Neogene surface is represented by deposits of the Upper Cretaceous and the Upper and Middle Jurassic ages. Along this horizon, there is a dip from the northeast to the southwest. The structural-tectonic model is complicated by thrusts, longitudinal shifts, normal and strike-slip faults, which divide the research area into separate blocks.

According to the structural constructions on the roof of the Tyrassian suite, against the background of the general rise of the horizon to the northeast in this part, a structural nose can be observed, which has a southeast extension.

A syncline can be traced along the Horodok flexure in the southwest along the horizons of the Lower Dashava subsuite and the roof of the Upper Dashava subsuite, within which there is a general coincidence of the structural plans of the mentioned horizons.

The difference in structural plans is observed in the area where the horizons adjoin the plane of the Horodok flexure.

The Northern Yavoriv structure of the semi-anticlinal type is mapped on the reflection seismic horizon of the roof of the Upper Dashava subsuite (VD-10). The structural and tectonic model of this horizon of the Northern Yavoriv area borders the Svydnytsia gas field through a syncline bend. According to the completed structural constructions along this horizon, as well as a complex comparison of methods, this area may represent a certain interest in terms of gas. It is recommended to drill well No. 1 on the Northern Yavoriv structure in order to search for Upper Dashava deposits.

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Keywords

structure, geoelectric section, geochemical anomaly, hydrocarbons, geological exploration works, Northern Yavoriv area

Referenses

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Duchuk, S. V., Maksymuk, S. V., & Halamai, A. R. (2023). Zastosuvannia kompleksnykh heofizychnykh i heokhimichnykh doslidzhen u poshukakh naftohazovykh skupchen v konteksti naroshchuvannia mineralno-syrovynnoi bazy Ukrainy. In Nadrokorystuvannia v Ukraini. Perspektyvy investuvannia: VIII Mizhnarodna naukovo-praktychna konferentsiia (Lviv, 9–12 zhovtnia 2023 r.) (pp. 308–312). Lviv. [in Ukrainian]

Duchuk, S. V., Yosypenko, T. M., & Maksymuk, S. V. (2018). Naftohazoperspektyvnist Latorytskoi ploshchi Zakarpatskoho prohynu za danymy kompleksnykh (heofizychnykh i heokhimichnykh doslidzhen). In Naftohazova haluz: Perspektyvy naroshchuvannia resursnoi bazy: tezy dopovidei Mizhnarodnoi naukovo-tekhnichnoi konferentsii (pp. 34–35). Ivano-Frankivsk. [in Ukrainian]

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ON THE SIGNIFICANCE OF NATURAL CARBONATES IN THE PROCESSES OF SYNTHESIS AND GENESIS OF HYDROCARBONS IN THE EARTH’S LITHOSPHERE

Home > Archive > No. 3–4 (191–192) 2023 > 135–142

Geology & Geochemistry of Combustible Minerals No. 3–4 (191–192) 2023, 135–142

https://doi.org/10.15407/ggcm2023.191-192.135

Josyp SVOREN’

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 fundamental importance of studies of the processes of synthesis and genesis of hydrocarbons in the Earth’s lithosphere has been confirmed and the prospects of the chosen direction for advanced research have been demonstrated, as well as for the thorough development of genetic principles of physical and chemical conditions of the formation of hydrocarbons deposits in various geological minds, focusing on the role of natural carbonate formation in this process. It is shown in this connection that one of the most striking natural phenomena of the Earth’s lithosphere is the obvious manifestations of veinlet-impregnated carbonate mineralization. This has been discussed in detail in the case of some areas of the Ukrainian Carpathians and Pre-Сarpathians, where the original carbonate veinlets of hydrothermal origin with traces of hydrocarbons migration are often happened, but industrial research works is rarely carried out because of their low (as expected) prospects for gas and oil deposits. We pay attention to the areas of development of the calcite veinlets with rare, perfectly faceted crystals of quartz – “Marmarosh diamonds” among the Cretaceous and Paleogene deposits of the South-Western slope of the Carpathians.

As a result, supporting materials on the importance of natural carbonates in the processes of synthesis and genesis of hydrocarbons in the Earth’s lithosphere are given. It consists in the revealed previously unknown property of natural carbonates, mainly calcium carbonate, under the action of abiogenic high-thermobaric deep fluid to decompose and be an additional source of carbon with different isotopic compositions in the processes of synthesis and genesis of hydrocarbons: gas, oil, bitumen as well as a carrier of these compounds in time of their migration and conservation in new creations in the deposits of oil and gas-bearing areas and metallogenic provinces: deposits-fields, veins, fluid inclusions, veinlet-impregnated mineralization.

Full Text

Keywords

fluid inclusions, carbonates, veins, hydrocarbons, deposits, gas and oil, mass spectrometric studies, supposed scientific discovery

Referenses

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Naumko, I. M. (2006). Fliuidnyi rezhym mineralohenezu porodno-rudnykh kompleksiv Ukrainy (za vkliuchenniamy u mineralakh typovykh parahenezysiv) [Extended abstract of Doctorʼs thesis, Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine]. Lviv. [in Ukrainian]

Naumko I., Bratus M., Dudok I., Kaliuzhnyi V., Kovalyshyn Z., Sakhno B., Svoren Y., & Telepko L. (2004). Fliuidnyi rezhym katahenno-hidrotermalnoho protsesu periodu formuvannia zhylnoi, prozhylkovoi i prozhylkovo-vkraplenoi mineralizatsii v osadovykh tovshchakh. In V. V. Kolodii (Ed.), Karpatska naftohazonosna provintsiia (pp. 308–345). Lviv; Kyiv: Ukrainskyi vydavnychyi tsentr. [in Ukrainian]

Naumko, I. M., & Svoren, Y. M. (2008). Pro shliakhy vtilennia hlybynnoho vysokotemperaturnoho fliuidu v zemnu koru. Dopovidi NAN Ukrainy, 9, 112–114. [in Ukrainian]

Svoren, I. M. (1984). Primesi gazov v kristallakh mineralov i drugikh tverdykh telakh, ikh sposoby izvlecheniya, sostav, forma nakhozhdeniya i vliyaniye na svoystva veshchestv [Extended abstract of Candidateʼs thesis. Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine]. Lvov. [in Russian]

Svoren, I. M. (1988). Formy nakhozhdeniya vodoroda v nekotorykh tverdykh materialakh razlichnogo proiskhozhdeniya soglasno fiziko-khimicheskoy modeli navodorozhivaniya tverdykh tel. In Geokhimiya i termobarometriya endogennykh flyuidov (pp. 95–103). Kiev: Naukova dumka. [in Russian]

Svoren, Y. M. (1992). Pytannia teorii henezysu pryrodnykh vuhlevodniv ta shliakhy poshuku yikh pokladiv. In Tektohenez i naftohazonosnist nadr Ukrainy (pp. 143–145). Lviv. [in Ukrainian]

Svoren, Y. (2020a). Nadra Zemli – pryrodnyi fizyko-khimichnyi reaktor: pryroda vody naftovykh i hazovykh rodovyshch. In Naftohazova haluz: Perspektyvy naroshchuvannia resursnoi bazy: materialy dopovidei Mizhnarodnoi naukovo-tekhnichnoi konferentsii (Ivano-Frankivsk, 8–9 hrudnia 2020 r.) (pp. 158–160). Ivano-Frankivsk: IFNTUNH. [in Ukrainian]

Svoren, J. M. (2020b). Various Chemical Properties of Carbon Isotopes in Natural Synthesis of Different Compounds. Journal of Geological Resource and Engineering, 8, 20–23. https://doi.org/10.17265/2328-2193/2020.01.002

Svoren, Y. M., & Davydenko, M. M. (1995). Termobarometriia i heokhimiia haziv prozhylkovo-vkraplenoi mineralizatsii u vidkladakh naftohazonosnykh oblastei i metalohenichnykh provintsii. Dopovidi NAN Ukrainy, 9, 72–73. [in Ukrainian]

Svoren, Y. M., Davydenko, M. M., Haievskyi, V. H., Krupskyi, Yu. Z., & Pelypchak, B. P. (1994). Perspektyvy termobarometrii i heokhimii haziv prozhylkovo-vkraplenoi mineralizatsii u vidkladakh naftohazonosnykh oblastei i metalohenichnykh provintsii. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4(88–89), 54–63. [in Ukrainian]

Svoren, Y. M., & Naumko, I. M. (2003). Nova teoriia syntezu i henezysu vuhlevodniv u litosferi Zemli: abiohenno-biohennyi dualizm. In Mezhdunarodnaya konferentsiya “Krym–2003” (pp. 75–77). Simferopol. [in Ukrainian]

Svoren, Y., & Naumko, I. (2004). Termobarometriia i heokhimiia haziv prozhylkovo-vkraplenoi mineralizatsii u vidkladakh naftohazonosnykh oblastei i metalohenichnykh provintsii: henezys i syntez prozhylkovykh karbonatnykh porid. In Mineralohiia: istoriia, teoriia i praktyka: tezy dopovidei Mizhnarodnoi naukovoi konferentsii, prysviachenoi 140-richchiu kafedry mineralohii Lvivskoho natsionalnoho universytetu imeni Ivana Franka (Lviv–Shatsk, 3–6 veresnia 2004 r.) (pp. 63–65). Lviv: Vydavnychyi tsentr LNU imeni Ivana Franka. [in Ukrainian]

Svoren, Y. M., & Naumko, I. M. (2005). Termobarometriia i heokhimiia haziv prozhylkovo-vkraplenoi mineralizatsii u vidkladakh naftohazonosnykh oblastei i metalohenichnykh provintsii – pryrodnyi fenomen litosfery Zemli. Dopovidi NAN Ukrainy, 2, 109–113. [in Ukrainian]

Svoren, Y. M., & Naumko, I. M. (2006). Nova teoriia syntezu i henezysu pryrodnykh vuhlevodniv: abiohenno-biohennyi dualizm. Dopovidi NAN Ukrainy, 2, 111–116. [in Ukrainian]

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ON THE REGULARITY OF NATURAL PROCESSES OF SYNTHESIS AND GENESIS HYDROCARBONS AND WATER OF OIL AND GAS FIELDS: ABIOGENIC-BIOGENIC DUALISM

Home > Archive > No. 1–2 (189–190) 2023 > 81–91

Geology & Geochemistry of Combustible Minerals No. 1–2 (189–190) 2023, 81–91

https://doi.org/10.15407/ggcm2023.189-190.081

Yosyp SVOREN’

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

Abstract

It is shown that the problem of the nature of water in oil and gas fields must be solved in an inextricable connection with the genesis and synthesis of natural hydrocarbons in the Earth’s bowels. The work offers an original solution, based on a new theory of the synthesis and genesis of hydrocarbons (oil, gas, etc.): abiogenic-biogenic dualism, which asserts that giant and supergiant oil and gas fields were formed from inorganic and organic original hydrocarbon-containing substances under the influence of abiogenic high-thermobaric deep fluid in harsh physical, physicochemical and geological conditions of the earth’s crust. Since the abiogenic high-thermobaric deep fluid contains hydrogen H+ and OH-containing anions, the described mechanism for the interaction of positively charged ions: C+, H+, CnHm+-radicals with the formation-synthesis of a complex hydrocarbon mixture such as gas, oil, bitumen, etc. must be logically supplemented by a reaction: Н2О → Н+ + ОН−. As a result of this complex physical and chemical process, the maximum concentration of (OH−) anions accumulated in the oxidation zone, which after the disappearance of the electric field become neutral and interact with each other according to the scheme: ОН + ОН = Н2О2 – hydrogen peroxide, which is an unstable compound, which decomposes into Н2О + О. Oxygen atoms became the starting substances for the formation of macro- and microcracks in these cavities under harsh conditions of rocks of the carbonate or quartz-carbonate type, etc., much less often – perfect mineral crystals, which with their defects in the process of growth (synthesis) captivate and preserve substances in the system (proper hydrocarbons and water). Тherefore, it was established for the first time that the natural water of oil and gas fields has a dual lithospheric-asthenospheric nature, while the lithospheric part is dominant, the isotopic composition is a mixture of these waters, and the deuterium isotope is more chemically active in complex physical and chemical processes, which run through the bowels of the planet. The obtained original data will contribute to the solution of Ukraine’s serious problem with energy carriers: natural gas, oil, coal and drinking water.

Full Text

Keywords

fluid inclusions, hydrocarbons, drinking water, energy carriers, oil and gas industry, fundamental science, scientific discoveries

Referenses

Bratus, M. D., Davydenko, M. M., Zinchuk, I. M., Kaliuzhnyi, V. A., Matviienko, O. D., Naumko, I. M., Pirozhyk, N. E., Redko, L. R., & Svoren, Y. M. (1994). Fliuidnyi rezhym mineraloutvorennia v litosferi (v zviazku z prohnozuvanniam korysnykh kopalyn). Kyiv: Naukova dumka. [in Ukrainian]

Dolenko, G. N. (1975). Sovremennoye sostoyaniye problemy proiskhozhdeniya nefti i gaza i formirovaniya ikh promyshlennykh zalezhey. In Zakonomernosti obrazovaniya i razmeshcheniya promyshlennykh mestorozhdeniy nefti i gaza (pp. 3–17). Kiev: Naukova dumka. [in Russian]

Naumko, I. M. (2006). Fliuidnyi rezhym mineralohenezu porodno-rudnykh kompleksiv Ukrainy (za vkliuchenniamy u mineralakh typovykh parahenezysiv) [Extended abstract of Doctorʼs thesis]. Instytut heolohii i heokhimii horiuchykh kopalyn NAN Ukrainy. Lviv. [in Ukrainian]

Naumko, I., & Svoren, Y. (2021). Innovatsiini tekhnolohii poshukiv korysnykh kopalyn, osnovani na doslidzhenniakh fliuidnykh vkliuchen u mineralakh. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4(185–186), 92–108. https://doi.org/10.15407/ggcm2021.03-04.092 [in Ukrainian]

Pavliuk, I., Naumko, I., & Stefanyk, Yu. (2007, December 13). Heolohy-naukovtsi proty metanu-vbyvtsi. U Lvovi na Naukovii taky ye nauka. Ukraina i Chas, 50(286), 7.

Svoren, Y. M. (1975). Istochniki uglerodsoderzhashchikh gazov vklyucheniy. In Uglerod i ego soyedineniya v endogennykh protsessakh mineraloobrazovaniya (po dannym izucheniya flyuidnykh vklyucheniy v mineralakh): tezisy Respublikanskogo soveshchaniya (Lvov, sentyabr 1975 g.) (pp. 104–106). Lvov. [in Russian]

Svoren, I. M. (1984). Primesi gazov v kristallakh mineralov i drugikh tverdykh telakh, ikh sposoby izvlecheniya, sostav, forma nakhozhdeniya i vliyaniye na svoystva veshchestv [Extended abstract of Candidateʼs thesis]. Institut geologii i geokhimii goryuchikh iskopayemykh AN USSR. Lvov. [in Russian]

Svoren. I. M. (1988). Formy nakhozhdeniya vodoroda v nekotorykh tverdykh materialakh razlichnogo proiskhozhdeniya soglasno fiziko-khimicheskoy modeli navodorozhivaniya tverdykh tel. In Geokhimiya i termobarometriya endogennykh flyuidov (pp. 95–103). Kiev: Naukova dumka. [in Russian]

Svoren, Y. M. (1992). Pytannia teorii henezysu pryrodnykh vuhlevodniv ta shliakhy poshuku yikh pokladiv. In Tektohenez i naftohazonosnist nadr Ukrainy (pp. 143–145). Lviv. [in Ukrainian]

Svoren, Y. (2011). Nadra Zemli – pryrodnyi fizyko-khimichnyi reaktor: izotopy vuhletsiu pro pokhodzhennia planety Zemlia. Heolohiia i heokhimiia horiuchykh kopalyn, 1–2(154–155), 158–159. [in Ukrainian]

Svoren, Y. (2018). Vlastyvist hlybynnoho abiohennoho metanovmisnoho vysokotermobarnoho fliuidu utvoriuvaty vuhillia. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4(176–177), 105–109. [in Ukrainian]

Svoren, Y. (2019). Nadra Zemli – pryrodnyi fizyko-khimichnyi reaktor: rizna khimichna vlastyvist izotopiv vuhletsiu u pryrodnykh protsesakh syntezu riznykh spoluk. In Problemy heolohii fanerozoiu Ukrainy: materialy X Vseukrainskoi naukovoi konferentsii (do 95-richchia kafedry istorychnoi heolohii ta paleontolohii i 120-richchia vid narodzhennia Severyna Ivanovycha Pasternaka (Lviv, 9–11 zhovtnia 2019 r.) (pp. 64–67). Lviv: LNU imeni Ivana Franka. [in Ukrainian]

Svoren, Y. (2020a). Nadra Zemli – pryrodnyi fizyko-khimichnyi reaktor: pryroda vody naftovykh i hazovykh rodovyshch. In Naftohazova haluz: Perspektyvy naroshchuvannia resursnoi bazy: materialy dopovidei Mizhnarodnoi naukovo-tekhnichnoi konferentsii (Ivano-Frankivsk, 8–9 hrudnia 2020 r.) (pp. 158–160). Ivano-Frankivsk: IFNTUNH. [in Ukrainian]

Svoren, J. M. (2020b). Subsoil Natural Physico-Chemical Reactor: Regularity of Natural Processes of Synthesis of Perfect Diamond Crystals. Journal of Geological Resource and Engineering, 8(4), 133–136. https://doi.org/10.17265/2328-2193/2020.04.005

Svoren, J. M. (2021). Subsoil Natural Physico-chemical Reactor: The Property of Deep Abiogenic Methane-Containing High-Thermobaric Fluid to Form Coal Seams. Journal of Geological Resource and Engineering, 9(1), 25–28. https://doi.org/10.17265/2328-2193/2021.01.003

Svoren, Y. M., & Davydenko, M. M. (1995). Termobarometriia i heokhimiia haziv prozhylkovo-vkraplenoi mineralizatsii u vidkladakh naftohazonosnykh oblastei i metalohenichnykh provintsii. Dopovidi NAN Ukrainy, 9, 72–73. [in Ukrainian]

Svoren, Y. M., Davydenko, M. M., Haievskyi, V. H., Krupskyi, Yu. Z., & Pelypchak, B. P. (1994). Perspektyvy termobarometrii i heokhimii haziv prozhylkovo-vkraplenoi mineralizatsii u vidkladakh naftohazonosnykh oblastei i metalohenichnykh provintsii. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4(88–89), 54–63. [in Ukrainian]

Svoren, Y. M., & Naumko, I. M. (2003). Nova teoriia syntezu i henezysu vuhlevodniv u litosferi Zemli: abiohenno-biohennyi dualizm. In Mezhdunarodnaya konferentsiya “Krym–2003” (pp. 75–77). Simferopol. [in Ukrainian]

Svoren, Y. M., & Naumko, I. M. (2006). Nova teoriia syntezu i henezysu pryrodnykh vuhlevodniv: abiohenno-biohennyi dualizm. Dopovidi NAN Ukrainy, 2, 111–116. [in Ukrainian]

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INNOVATIVE TECHNOLOGIES OF THE PROSPECTING FOR MINERAL DEPOSITS BASED ON DATA OF FLUID INCLUSIONS RESEARCH

Home > Archive > No. 3–4 (185–186) 2021 > 92–108

Geology & Geochemistry of Combustible Minerals No. 3–4 (185–186) 2021, 92–108.

https://doi.org/10.15407/ggcm2021.03-04.092

Ihor NAUMKO, Yosyp SVOREN

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 innovative approach to the development of prospective technologies (methods) was substantiated on crystallogenic and physicochemical principles of the knowledge of mineral forming environments (fluids) (thermobarogeochemistry – mineralofluidology – fluid inclusions) as a new branch of geological knowledge within the framework of the new scientific direction in the geology – “thermobarometry and geochemistry of gases of veinlet-impregnated mineralization in deposits of oil- and gas-bearing areas and metallogenic provinces” as a natural phenomenon of the Earth’s lithosphere. According to him, the creation of radically new technologies and realization of prospecting for mineral deposits (first of all hydrocarbons and gold) simultaneously with the elucidation of the problem of genesis and synthesis of hydrocarbons at the atomic-molecular level fixed by such defects in the mineral crystals as fluid inclusions. Developed technologies, namely: determination of genesis of hydrocarbon gases; determination of prospects of oil and gas presence of a local area; local forecast of enriched areas of gold ore fields; express determination of potassium ions in inclusions for identification of gold-enriched and barren veinlet formations, – belong to the branch of the exploration geology and geochemistry and are used to ascertain genetic guestions, to solve tasks of the mineralogical-geochemical prediction and prospecting for mineral deposits in the local structures of oil- and gas-bearing areas and metallogenic provinces. The comparison of fluid inclusions of veinlets and host rocks based on the sections of a number of wells has shown the considerable possibilities of the developed technologies and prospects of the usage of thermobarogeochemical-mineralofluidological indicators in the complex with the geochemical and geophysical (petrophysical) methods, data of geological survey, deep-seated drilling while predicting hydrocarbon deposits in the local structures of the sedimentary strata promising for oil and gas and making necessary amendments in the directions of the following geological-prospecting works.

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Keywords

innovative technologies, fluid inclusions, geochemistry, thermobarometry, fluids, hydrocarbons, gold, mineral-ore-naphthidogenesis, Earth’s lithosphere

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PROSPECTS FOR OIL AND GAS PRESENCE OF LOWER SARMATIAN DEPOSITS IN THE NORTH-WESTERN PART OF THE OUTER ZONE OF THE CARPATHIAN FOREDEEP (by hydrogeochemical and hydrodynamic indicators)

Home > Archive > No. 3–4 (185–186) 2021 > 16–32

Geology & Geochemistry of Combustible Minerals No. 3–4 (185–186) 2021, 16–32.

https://doi.org/10.15407/ggcm2021.03-04.016

Halyna MEDVID, Olga TELEGUZ, Vasyl HARASYMCHUK, Maria KOST’, Solomiya KALMUK

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 hydrogeochemical parameters of the Lower Sarmatian aquifer of the north-western part of the Outer Zone of the Carpathian Foredeep have been studied. The waters of the chloride-calcium type (according to the classification of V. O. Sulin) are dominated. Other types of water are distributed locally. On the basis of the calculated genetic coefficients, the conclusion on sedimentogenic conditions of their forming during a geological history of the region is made.

It is established that the general tendency for the deposits of the Outer Zone is increasing of TDS of water with depth and stratigraphy. The waters of the north-western part of the Outer Zone are characterized by reduced values of sulfate content and sulfation coefficient rSO42– · 100/rCl–, indicating the conditions of hydrogeological closed structures.

The genetic index of formation water metamorphism (rNa+/rCl–) is mainly inversely dependent on TDS. Its values greater than one are inherent in waters of hydrocarbonate-sodium and sulfate-sodium types, which are not typical for the hydrocarbon deposits. The nature of fluctuations in the values of the chlorine-bromine coefficient is fully consistent with other hydrochemical parameters and the results of paleohydrodynamic reconstructions.

A detailed analysis of the current hydrodynamic situation of Lower Sarmatian aquifer in combination with geochemical features and paleohydrodynamic reconstructions allowed to identify the perspective structures of the studying region. Our forecasts for the gas potential of the Krukenychy depression are consistent with the forecasts of researchers of Ivano-Frankivsk National Technical University of Oil and Gas. The results of their research are based on gravitational field anomalies.

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Keywords

hydrogeological criteria, hydrogeochemical features, hydrocarbons, Outer Zone, Carpathian Foredeep

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Kolodii, V., Medvid, H., Harasymchuk, V., Pankiv, R., Velychko, N., & Dobushchak, M. (2006). Hidroheolohiia naftovykh i hazovykh rodovyshch Karpatskoi naftohazonosnoi provintsii. Chastyna I. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4, 140–159. [in Ukrainian]

Krupskyi, Yu. Z. (2001). Heodynamichni umovy formuvannia i naftohazonosnist Karpatskoho ta Volyno-Podilskoho rehioniv Ukrainy. Kyiv: UkrDHRI. [in Ukrainian]

Krupskyi, Yu. Z., Andreichuk, M. M., & Chepil, P. M. (2006). Obstanovky osadkonahromadzhennia v miotseni Zovnishnoi zony Peredkarpatskoho prohynu i naftohazonosnist. Heolohichnyi zhurnal, 2, 27–41. [in Ukrainian]

Maievskyi, B. Y., & Kurovets, S. S. (2016). Henezys vuhlevodniv i formuvannia yikh pokladiv yak osnova prohnozuvannia naftohazonosnosti hlybokozanurenykh horyzontiv osadovykh baseiniv. Heohrafiia i heolohiia. Sektsiia 13. https://www.sworld.com.ua/simpoz6/75.pdf [in Ukrainian]

Medvid, H. B. (2011). Hidroheokhimichni osoblyvosti nyzhnosarmatskykh vidkladiv Zovnishnoi zony Peredkarpatskoho prohynu. In Resursy pryrodnykh vod Karpatskoho rehionu (Problemy okhorony ta ratsionalnoho vykorystannia): materialy IX Mizhnarodnoi naukovo-praktychnoi konferentsii (Lviv, 19–20 travnia 2011 r.) (pp. 46–51). Lviv: LvTsNTEI. [in Ukrainian]

Medvid, H. (2013). Do pytannia genezy pidzemnykh vod ta formuvannia pokladiv hazu u miotsenovykh tovshchakh pivnichno-zakhidnoi chastyny Zovnishnoi zony. In Suchasni problemy heolohii: zbirnyk naukovykh prats do 155-richchia z dnia narodzhennia P. A. Tutkovskoho (Kyiv, 15–17 travnia 2013 r.) (pp. 312–317). Kyiv: Fiton. [in Ukrainian]

Medvid, H. (2018). Paleohidroheolohichna kharakterystyka miotsenu pivnichno-zakhidnoi chastyny Zovnishnoi zony Peredkarpatskoho prohynu. Heolohiia i heokhimiia horiuchykh kopalyn, 3–4(176–177), 73–85. [in Ukrainian]

Monchak, L. S., Anikeiev, S. H., Maievskyi, B. Y., & Kurovets, S. S. (2014). Pro perspektyvy hazonosnosti hlybokozanurenykh horyzontiv Krukenytskoi zapadyny. Naftohazova haluz Ukrainy, 3, 16–18. https://www.naftogaz.com/files/journal/3_2014_preview.pdf [in Ukrainian]

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Orlov, O. O., Loktiev, A. V., Trubenko, O. M. ta in. (2004). Formuvannia hazovykh pokladiv v tonkosharuvatykh pachkakh pishchano-hlynystoi tovshchi neohenu Zovnishnoi zony Peredkarpatskoho prohynu. In Nafta i Haz Ukrainy–2004: materialy VIII Mizhnarodnoi naukovo-praktychnoi konferentsii (Sudak, 29.09–01.10.2004) (pp. 215–218). Lviv: Tsentr Yevropy. [in Ukrainian]

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Vyshniakov, I. B., Vul, M. Ya., Honyk, I. O., Zurian, O. V., & Starynskyi, V. O. (2014). Suchasnyi stan vuhlevodnevoi syrovynnoi bazy Zakhidnoho naftohazonosnoho rehionu Ukrainy ta osnovni napriamy heolohorozviduvalnykh robit shchodo yii osvoiennia. Mineralni resursy Ukrainy, 4, 33–38. [in Ukrainian]

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GEOLOGICAL-GEOCHEMICAL FEATURES OF MIGRATION AND FORMATION OF GAS FIELDS IN OIL- AND GAS-BEARING REGIONS OF UKRAINE

Home > Archive > No. 1 (178) 2019 > 21-40

Geology & Geochemistry of Combustible Minerals No. 1 (178) 2019, 21-40.

https://doi.org/10.15407/ggcm2019.01.021

Olesya SAVCHAK

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

Abstract

Geochemical composition of main components of natural gas has been analysed for three oil- and gas-bearing regions of the Ukraine, namely: Western (40 fields of the Precarpathian deep, 4 gas fields of the Transcarpathian deep and 2 gas fields located within the limits of the Lviv Paleozoic deep), Eastern (composition of natural gases at 12 fields) and Southern (analysis of data on chemical composition of natural gases from 8 fields in the water area of the deep and 13 fields on land).

Comparative analysis of the composition of natural hydrocarbons has been carried out within the limits of the Western region based on the main structural-tectonic elements of the region: outer and inner zones of the Precarpathian deep, the Transcarpathian deep and the Lviv Paleozoic deep; within the Eastern region – the Northern edge of the deep and the deep itself; within the Southern region – water area and land. On this basis the definite zonality of the distribution of hydrocarbon components of natural gases within the bounds of the oil-gas regions has been determined. Such different composition of gases testifies to independent sources of hydrocarbon supply and different duration of migration of the latter.

The analyses of the features of the distribution of the components of natural gas of main oil- and gas-bearing regions of the Ukraine and of the gas presence in the aggregate have enabled us to determine main aspects of the processes both of lateral and vertical migration of hydrocarbons.

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Keywords

geochemical features, migration, hydrocarbons, Western, Eastern and Southern oil-gas regions of Ukraine.

REFERENCES

Atlas rodovyshch nafty i hazu Ukrainy. T. 4-5. Zakhidnyi naftohazonosnyi rehion. (1998). Lviv: UHNA. [in Ukrainian]
 
Pavliuk, M. I., Varichev, S. O., Rizun, B. P., & Savchak, O. Z. (2002). Naftohazonosni provintsii Ukrainy (heodynamichnyi aspekt). Heolohiia i heokhimiia horiuchykh kopalyn, 1, 3-12. [in Ukrainian]
 
Pavliuk, M. et al. (2008). Heodynamichni umovy formuvannia naftohazonosnykh provintsii Ukrainy. Heolohiia i heokhimiia horiuchykh kopalyn, 3 (144), 16-25. [in Ukrainian]
 
Savchak, O. Z. (2003). Heokhimichni osoblyvosti naft i kondensativ Pivdennoho naftohazonosnoho rehionu Ukrainy. Heolohiia i heokhimiia horiuchykh kopalyn, 3-4, 27-37. [in Ukrainian]
 
Savchak, O. Z. (2015). Heodynamichni aspekty roztashuvannia rodovyshch nafty i hazu naftohazonosnykh provintsii Ukrainy. In Heolohiia horiuchykh kopalyn: Materialy Mizhnar. nauk. konf. (Kyiv, 2-4 veresnia 2015 r.) (pp. 96-98). Kyiv. [in Ukrainian]
 
Savchak, O. Z. (2017a). Heokhimichni aspekty protsesiv naftohazonahromadzhennia naftohazonosnykh rehioniv Ukrainy. Heolohiia i heokhimiia horiuchykh kopalyn, 1-2 (170-171), 154-156. [in Ukrainian]
 
Savchak, O. Z. (2017b). Heokhimichni aspekty protsesiv mihratsii ta akumuliatsii vuhlevodniv Skhidnoho naftohazonosnoho rehionu Ukrainy. Heolohiia i heokhimiia horiuchykh kopalyn, 3-4 (172-173), 9-29. [in Ukrainian]
 
Savchak, O. Z. (2018). Heodynamichni ta heokhimichni aspekty naftohazonahromadzhennia Zakhidnoho naftohazonosnoho rehionu Ukrainy. Heolohiia i heokhimiia horiuchykh kopalyn, 3-4 (176-177), 5-20. [in Ukrainian]
 
Savchak, O. Z. (2019). Heoloho-heokhimichni osoblyvosti rozmishchennia rodovyshch nafty i hazu naftohazonosnykh provintsii Ukrainy. In Tezy dop. Nauk. konf., prysviachenoi 50-richchiu In-tu heokhimii, mineralohii ta rudoutvorennia im. M. P. Semenenka NAN Ukrainy (Kyiv, 14-16 travnia 2019 r.) (T. 2, pp. 82-84). Kyiv. [in Ukrainian]
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HYDROGEN AS A SOURCE OF ENERGY AND GEODYNAMIC PROCESSES

Home > Archive > No. 3-4 (176-177) 2018 > 85-104

Geology & Geochemistry of Combustible Minerals No. 3-4 (176-177) 2018, 85-104.

Ihor BAGRIY, Stanislav KUZMENKO

Institute of Geological Sciences of National Academy of Sciences of Ukraine, Kyiv, e-mail: bagrid@ukr.net

Dmytro GUNYA

SS “Volodarske” PJSC “Mine named after O. F. Zasiadko”, Kharkiv, e-mail: dmytrogunia53@gmail.com

Abstract

Long-term results of research on mapping oil and gas bearing sites at traditional and non-traditional sites (mine fields, shelf zones, astroblems) have made it possible to create a database of systemic criteria for search technology of structural thermo-atmo-hydrological and geochemical research, where for the first time in the search practice hydrogen was used as the main component of the hydrocarbons. Analysis of the results of the data on the distribution of hydrogen concentrations made it possible to isolate abnormal values both in areas and in productive wells (in the absence of background) and conduct detailed large-scale area studies for the purpose of area mapping for prospecting.

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Keywords

cycle; hydro-geosynergetic biogenic-mantle theory, hydrocarbons, structural thermo-atmo-hydrological and geochemical research.

Referenses

Babinets, A. E. (1961). Podzemnye vody yugo-zapada Russkoi platformy. Kiev: Izdatel’stvo AN USSR. [in Russian]
 
Babinets, A. E., & Belyavskii, G. A. (1973). Estestvennye resursy podzemnykh vod zony intensivnogo vodoobmena Ukrainy. Kiev: Naukova dumka. [in Russian]
 
Bagrii, I. D. (2016). Gidro-geosinergeticheskaya biogenno-mantiinaya gipoteza obrazovaniya uglevodorodov i ee rol’ pri obosnovanii pryamopoiskovoi tekhnologii. Geologicheskii zhurnal, 2 (355), 107-133. [in Russian]
 
Bahrii, I. D. (2003). Prohnozuvannia rozlomnykh zon pidvyshchenoi pronyknosti hirskykh porid dlia vyrishennia heoekolohichnykh ta poshukovykh zadach. Kyiv: Vydavnychyi dim Dmytra Buraho. [in Ukrainian]
 
Bahrii, I. D. (2013). Rozrobka heoloho-strukturno-termo-atmoheokhimichnoi tekhnolohii prohnozuvannia poshukiv korysnykh kopalyn ta otsinky heoekolohichnoho stanu dovkillia. Kyiv: Lohos. [in Ukrainian]
 
Bahrii, I. D., Hozhyk, P. F., Pochtarenko, V. I., Aksom, S. D., Dubosarskyi, V. R., Mamyshev, I. Ye., Kizlat, A. M., & Palii, V. M. (2011). Prohnozuvannia heodynamichnykh zon ta perspektyvnykh ploshch dlia vydobutku shakhtnoho metanu vuhilnykh rodovyshch Donbasu. Kyiv: Foliant. [in Ukrainian]
 
Belousov, V. V. (1966). Zemnaya kora i verkhnyaya mantiya materikov. Moskva: Nauka. [in Russian]
 
Chekalyuk, E. B. (1967). Neft’ verkhnei mantii Zemli. Kiev: Naukova dumka. [in Russian]
 
Dolenko, G. N. (1962). Geologiya nefti i gaza Karpat. Kiev: Izdatel’stvo AN USSR. [in Russian]
 
Grinberg, I. V. (1971). Nekotorye khimicheskie aspekty problemy genezisa teorii. In Problema proiskhozhdeniya nefti i gaza i formirovanie ikh promyshlennykh zalezhei (s. 52-67). Kiev: Naukova dumka. [in Russian]
 
Gutenberg, B. (1957). Skorosti rasprostraneniya seismicheskikh voln v zemnoi kore. In A. Poldervart (Ed.). Zemnaya kora (s. 121-138). Moskva: Izdatel’stvo inostrannoi literatury. [in Russian]
 
Krayushkin, V. A., & Kutcherov, V. G. (2010). Deep-seated abiogenic origin of petroleum: From geological assessment to physical theory. Reviews of Geophysics, 48 (1), 1-30.
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Magnitskii, V. A. (1965). Vnutrennee stroenie i fizika Zemli. Moskva: Nedra. [in Russian]
 
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Porfir’ev, V. B., & Grinberg, I. V. (1966). Sovremennoe sostoyanie teorii organicheskogo proiskhozhdeniya nefti. In Problemy proiskhozhdeniya nefti (s. 5-51). Kiev: Naukova dumka. [in Russian]
 
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Subbotin, O. I., Naumchik, G. L., & Rakhimova, N. T. (1964). Protsessy v verkhnei mantii Zemli i svyaz’ s nimi stroeniya zemnoi kory. Kiev: Naukova dumka. [in Russian]
 
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Vernadskii, V. I. (2001). Khimicheskoe stroenie biosfery Zemli i ee okruzheniya. Moskva: Nauka. [in Russian]
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ESTIMATION OF PROSPECTS FOR OIL AND GAS PRESENCE IN THE LAZESHCHINA AREA OF THE KROSNO ZONE OF THE CARPATHIANS BASED ON DATA OF COMPLEX GEOLOGICAL-GEOPHYSICAL STUDIES

Home > Archive > No. 3-4 (176-177) 2018 > 63-72

Geology & Geochemistry of Combustible Minerals No. 3-4 (176-177) 2018, 63-72.

Sofia MAKSYMUK

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

Petro BODLAK

West Ukrainian Geophysical Prospecting Expedition, Lviv, e-mail: zugre@lviv.farlep.net

Taras YOSYPENKO

West Ukrainian Geophysical Prospecting Expedition, Lviv, e-mail: zugre@lviv.farlep.net

Abstract

A complex of geophysical and geochemical studies was conducted in the Krosno zone on Lazeshchina area. Three layers of the anticlinal structures of the Carpathian Stretch – Yasinia, Lazeshchina and Stebnyk were traced in the structural plane. According to the seismic horizon P3c they have the form of brachiaticlinal folds, limited from the south and the north by the deep thrusts of the amplitude from 200 to 220 m. The presence of a significant number of tectonic elements resulted in a strong fracturing of the allochton, making it fluid-permeable for gaseous migrants.

According to the results of electrical survey the boundaries of Dovzhynets, Vyhoda, Bystrytsia and Manyava suites are clearly traced. The zones of increased resistance in Dovzhynets, Vyhoda suites (profile 1285904) and in the Golovetsko suite (profile 1295904) may be associated with oil and gas saturation of rocks.

Geochemical studies have established the composition of hydrocarbon mixtures of near-surface sediments, maps of the distribution of geochemical parameters with the allocation of zones of manifestation of their abnormal concentrations have been constructed.

Geochemical anomalies are well connected with structural buildups in the Yasinia, and Stebnyk folds. In addition, in the eastern and southeastern parts of the area, two more fields of abnormal concentrations of hydrocarbon components not covered by seismic exploration are identified. An important argument of its possible fluid saturation is the complexity of the geochemical anomaly, so this part of the area may have an important search value in the future.

Priority for conducting exploration works should be Yasynia fold, with localization of which are coincided with geochemical anomalies and increased resistance in geoelectrical profiles. The obtained results testify to oil and gas prospects of this area and the possibility of discovering new hydrocarbon deposits in the Krosno zone.

Full Text

Keywords

structure, geoelectrical profile, geochemical anomaly, hydrocarbons, флюїдонасиченість, exploration works, Lazeshchina area.

Referenses

Bilichenko, V. Ya. (1999). Strukturno-tektonichni osoblyvosti paraavtokhtonu Ukrainskykh Karpat ta prylehlykh terytorii za materialamy detalnoi hravimetrii. Heolohiia i heokhimiia horiuchykh kopalyn, 3, 131-138. [in Ukrainian]
 
Devid, Dzh. (1990). Statisticheskii analiz dannykh v geologii (T. 1-2). Moskva: Nedra. [in Russian]
 
Glushko, V. V., & Kruglov, S. S. (Red.). (1986). Tektonicheskaya karta Ukrainskikh Karpat. Masshtab 1 : 200 000. – L’vov: UkrNIGRI. [in Russian]
 
Kolodii, V. V., Boiko, H. Yu., & Boichevska, L. E. ta in. (2004). Karpatska naftohazonosna provintsiia. Lviv; Kyiv: Ukrainskyi vydavnychyi tsentr. [in Ukrainian]
 
Krupskyi, Yu. Z. (2001). Heodynamichni umovy formuvannia i naftohazonosnist Karpatskoho ta Volyno-Podilskoho rehioniv Ukrainy. Kyiv: UkrDHRI. [in Ukrainian]
 
Krupskyi, Yu. Z. (Head). (2002). Utochnennia heolohichnoi budovy Bitlianskoho i Turkivskoho subpokryviv Karpat (zona Krosno) za danymy heolohichnykh ziomok i tematychnykh robit z metoiu vyiavlennia naftohazoperspektyvnykh obiektiv (№ D8/02). Lviv. [in Ukrainian]
 
Krupskyi, Yu. Z., & Krupska, O. Yu. (2008). Vydilennia perspektyvnykh terytorii dlia poshuku rodovyshch zi znachnymy zapasamy vuhlevodniv u Zakhidnomu naftohazonosnomu rehioni. Heolohiia i heokhimiia horiuchykh kopalyn, 1 (142), 5-11. [in Ukrainian]
 
Krupskyi, Yu. Z., Kurovets, I. M., & Senkovskyi, Yu. M. ta in. (2014). Netradytsiini dzherela vuhlevodniv Ukrainy. Kn. 2. Zakhidnyi naftohazonosnyi rehion. Kyiv: Nika-Tsentr. [in Ukrainian]
 
Kudla, P. Y. (2004). Zvit pro rezultaty poshukovykh seismorozviduvalnykh robit MSHT na Lazeshchynskii ploshchi Krosnenskoi zony (№ 2052). Lviv: ZUHRE. [in Ukrainian]
 
Kurovets, I. M., Krupskyi, Yu. Z., & Naumko, I. M. ta in. (2011). Perspektyvy poshukiv pokladiv vuhlevodniv u vidkladakh olihotsenu zony Krosno (Ukrainski Karpaty). Heodynamika, 2 (11), 144-146. [in Ukrainian]
https://doi.org/10.23939/jgd2011.02.144
 
Makitra, R. H., & Semeniuk, M. V. (2014). Do istorii doslidzhen i vykorystannia nafty Prykarpattia. In Aktual’nye problemy poiskovoi i ekologicheskoi geokhimii: tezisy dokladov Mezhdunarodnoi nauchnoi konferentsii (s. 74-77). Kiev. [in Ukrainian]
 
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Orlov, O. O., & Kalynii, Yu. A. (2011). Perspektyvy poshukiv i rozvidky pokladiv vuhlevodnevykh enerhonosiiv v Krosnenskii zoni Skladchastykh Karpat. Naukovyi visnyk Ivano-Frankivskoho natsionalnoho tekhnichnoho universytetu nafty i hazu, 4, 5-10. [in Ukrainian]
 
Polivtsev, A. V., Pomortsev, G. P., & Borkovskii, A. A. (1990). Gazogeokhimicheskie poiski poleznykh iskopaemykh v Karpatskom regione. Kiev: Naukova dumka. [in Russian]
 
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GEODYNAMIC AND GEOCHEMICAL ASPECTS OF OIL AND GAS ACCUMULATION OF THE WESTERN OIL AND GAS REGION OF UKRAINE

Home > Archive > No. 3-4 (176-177) 2018 > 5-20

Geology & Geochemistry of Combustible Minerals No. 3-4 (176-177) 2018, 5-20.

Olesya SAVCHAK

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

Abstract

The Western oil-gas region of Ukraine is the most important oil- and gas-producing region of Ukraine and is the oldest one as to the time of discovery of commercial deposits of hydrocarbons. In all 94 fields were discovered in the region. Six of them belong to great, eight – to middle and eighty – to small. The greatest amount of fields is in the Bilche-Volytsa (47) and the Boryslav-Pokuttya (39) oil-gas regions. In the Transcarpathian gas-bearing region five gas fields are known, in the Carpathian – two oil fields and within the limits of the Volyn-Podillya area – two gas fields. We have analysed the geochemical composition of oil and condensate for 3 structural-tectonic elements of the region: outer, inner zone of the Carpathian Foredeep and Folded Carpathians and the comparative analysis of the composition of natural hydrocarbons within the limits of the region was carried out. The analysis of peculiarities of the geological structure and oil and gas presence in the totality with available geochemical data has allowed us to come to a conclusion that formation of oil and gas deposits in the Western oil- and gas-bearing region is caused both lateral and vertical migration of hydrocarbons.

Full Text

Keywords

geochemical features, migration, hydrocarbons, Western oil and gas region of Ukraine.

Referenses

Dolenko, G. N. (1990). Geologiya i geokhimiya nefti i gaza. Kiev: Naukova dumka. [in Russian]

Ivaniuta, M. M. (Ed.). (1998). Atlas rodovyshch nafty i hazu. T. 4–5. Zakhidnyi naftohazonosnyi rehion. Lviv. [in Ukrainian]

Pavliuk, M., Halabuda, M., Rizun, B. et al. (2008). Heodynamichni umovy formuvannia naftohazonosnykh provintsii Ukrainy. Heolohiia i heokhimiia horiuchykh kopalyn, 3 (144), 16–25. [in Ukrainian]

Savchak, O. Z. (2015). Heodynamichni aspekty roztashuvannia rodovyshch nafty i hazu naftohazonosnykh provintsii Ukrainy. In Heolohiia horiuchykh kopalyn: materialy Mizhnarodnoi naukovoi konferentsii (Kyiv, 2–4 veresnia 2015 r.) (s. 96–98). Kyiv. [in Ukrainian]

Savchak, O. Z. (2017). Heokhimichni aspekty protsesiv naftohazonahromadzhennia naftohazonosnykh rehioniv Ukrainy. Heolohiia i heokhimiia horiuchykh kopalyn, 1–2 (170–171), 154–156. [in Ukrainian]

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GEOLOGICAL, STRUCTURAL AND GEOCHEMICAL FEATURES GENERATION OF HYDROCARBONS OF THE SRIBNYANSKA DEPRESSION

Home > Archive > No. 1-2 (174-175) 2018 > 40-53

Geology & Geochemistry of Combustible Minerals No. 1-2 (174-175) 2018, 40-53.

Vitaliy GLON

Institute of Geological Sciences of National Academy of Sciences of Ukraine, Kyiv, е-mail: italiyglon@gmail.com

Abstract

Complex researches are conducted on the territory of the Sribnyanska depression. Systematic analysis of structural-thermal-atmogeochemical researches of oil and gas perspective objects of the Dnieper-Donetsk Rift was carried out. Interpretation and generalization of the received data was carried out. Criteria of oil and gas prospective formation complexes have been described. Based on the distribution of criteria of structural-thermal-atmogeochemical researches, prospects areas for the search of hydrocarbons within the limits of the Sribnyanska depression have been identified.

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Keywords

Dnieper-Donetsk Rift, Sribnyanska depression, oil and gas prospects, anomalies, hydrocarbons.

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