fluids – Geology and Geochemistry of Combustible Minerals

Posted on November 2021June 2022 by GGCMJournal

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.

Full Text

Keywords

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

Referenses

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Posted on January 2020May 2021 by GGCMJournal

GEOCHEMISTRY AND THERMOBAROMOMETRY OF MINERAL-FORMING FLUIDS AND THERMOBAROGEOCHEMISTRY OF EVAPORITES – WORLD-FAMOUS SCIENTIFIC SCHOOLS

Home > Archive > No. 1 (182) 2020 > 62-75

Geology & Geochemistry of Combustible Minerals No. 1 (182) 2020, 62-75.

https://doi.org/10.15407/ggcm2020.01.062

Ihor NAUMKO, Myroslav PAVLYUK, Andriy POBEREZHSKYY
Institute of Geology and Geochemistry of Combustible Minerals of National Academy of Sciences of Ukraine, Lviv, e-mail: igggk@mail.lviv.ua

Abstract

Fundamental and applied achievements in the fields of geochemistry and thermobarometry of mineral-forming fluids and thermobarogeochemistry of evaporites are summarized as the basis of the corresponding world-famous scientific thermobarogeochemical schools established by professors V. A. Kalyuzhny and O. Yo. Petrychenko at the Institute of Geology and Geochemistry of Combustible Minerals of the Academy of Sciences of Ukraine on the basis of creative development of ideas of predecessors with the support of academicians Ye. K. Lazarenko, V. S. Sobolyev, H. N. Dolenko. Emphasis is placed on the contribution of schools to geological science, which is determined by the formed knowledge base on geochemical and thermobaric parameters of fluid environments of mineral-ore- naphthidogenesis in the Earth’s lithosphere (according to data of fluid inclusions research). In this context, in view of the enormous array of available data, the composition, physicochemical properties, genesis of fluids of the upper mantle and crust are briefly discussed and it is shown that the course of processes of petro-, mineral-, ore-, naphthidogenesis and formation fields of hydrocarbon, ore and non-ore minerals is determined by the peculiarities of degassing (defluidization) of the Earth and its influence on the conversion of carbon compounds during terrigenous, organogenic, hemogenic sedimentation and on the processes of diagenesis of sediments of various origins. The obtained data on the reproduction of the evolution of the fluid regime of rock complexes contribute to solving the fundamental problem of geochemistry of carbon and hydrogen (hydrocarbon-hydrogen matter) and deep (endogenous) fluid flows in the Earth’s lithosphere as an important basis for mineralofluidological model of the planet. They played a decisive role in substantiating at the Institute on the basis of abiogenic-biogenic dualism universal approaches to the processes of synthesis and genesis of natural hydrocarbons in the form of a new fundamental paradigm of oil and gas geology and geochemistry, the polygenesis of natural hydrocarbons in the Earth’s bowels, which increases the potential of oil and gas resources of promising regions, including Ukraine. This creates the preconditions for the identification of promising rock complexes for hydrocarbon, ore and non-ore minerals by applying the obtained fundamental thermobarogeochemical data in forecasting, exploration and operational practice on the basis of developing of new non-traditional geotechnologies for assessment and exploration of hydrocarbons and minerals.

Full Text

Keywords

fluid inclusions, geochemistry, thermobarometry, fluids, fluid media, mineral-ore-naphthidogenesis, Earth’s lithosphere.

REFERENCES

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Posted on December 2019May 2021 by GGCMJournal

ON THE LITHOFLUID AHD THERMODYNAMIC SYSTEM IN GEOLOGY AND GEOCHEMISTRY

Home > Archive > No. 2 (179) 2019 > 28-36

Geology & Geochemistry of Combustible Minerals No. 2 (179) 2019, 28-36.

https://doi.org/10.15407/ggcm2019.02.028

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

Abstract

The researcher’s approaches to the term “fluid systems” as a prototype of the fluid medium of crystallization of minerals, naturally preserved relics – inclusions of fluids reflect the features of the fluid regime of mineralogenesis of rock-ore complexes are analyzed. It is emphasized that the term “fluid” characterizes the main property of the substance of the medium of mineralogenesis, the most important substance of the Earth’s crust, its highest mobility, the maximum disorder of structure, fluidity, and covers the liquid or gas state of the lightweight components (gas, aqueous solution), as well as the melt of magmatic (silicate, salt, carbonate) substance. Under the fluid regime, the author understands the physical and chemical nature, the spatial-temporal sequence of manifestation and the variability of the parametric characteristics of the fluids, that is, the entire set of physico-chemical and geological phenomena and processes that determine the regular (discrete, periodic, evolutionary) changes in aggregate state, PT-parameters and the composition of the fluid medium of crystallization of minerals and their identified (certain, specific) parageneses. Our long-term studies show that the physico-chemical system of the fluid medium of mineral-ore-narhtidgenesis should cover lithoid (rocky), fluid (genetic) and thermodynamic (temperature, pressure, concentration) components that determine the mass, heat and the energy exchange between the fluid and of its host rock. In view of this, we define this physico-chemical system as a “lithofluid and thermodynamic system” and we believe that this definition takes into account all known phenomena of generation, migration, differentiation and accumulation of fluids, in particular hydrocarbons (hydrocarbon-containing), in the lithosphere of the Earth. An example of such a lithofluid and thermodynamic system in the Earth’s bowels – the natural high-energy physicochemical reactor is the hydrocarbon-generating and mineral-ore-forming system of the deep abiogenic high-termobaric fluid.

Full Text

Keywords

inclusion in minerals, fluid systems, fluids, fluid regime, lithofluid and thermodynamic system, lithosphere of the Earth.

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