Pub Date : 2020-01-01DOI: 10.15407/mineraljournal.42.04.069
O. Mytrokhyn, V. Bakhmutov, A. Aleksieienko, T. Mytrokhina
The Anagram Islands are located near the Graham Coast of West Antarctica not far from the Ukrainian Antarctic Station "Akademik Vernadsky". Gabbroids that are probably Cretaceous in age predominate in the geological structure of the Anagram Islands. New data on the mode of occurrence of the Anagram gabbroids and their layering were obtained during the seasonal field works of the Ukrainian Antarctic Expeditions in 2017, 2019-2020 years. Samples of the gabbroids were examined by optical microscopy, electron microscopy and microprobe analysis as well as by measuring of anisotropy of magnetic susceptibility of rocks. The goal of the research was to clarify the geological position and petrographic features of the Anagram gabbroids, to determine the typomorphic features of rock-forming minerals, and to clarify the origin of the layering in gabbroids. It was determined that the bottom part of a large layered gabbroid intrusion is fragmentarily exposed on the Anagram Islands. The continuation of the intrusion is expected in the northeastern and southeastern directions. It was established that primary magmatic textures and mineral composition are preserved in the gabbroids despite the development of metamorphic amphibolization. The gabbroids show typical cumulative textures of magmatic origin. The main cumulative phases are plagioclase (An70-95), clinopyroxene (Wo41-49En34-47), orthopyroxene (Wo2-4En49-71), olivine (Fo67-69), Ti-magnetite and ilmenite. It is proved that the fine rhythmic-gradational layering in the gabbroids was formed by gravitational precipitation of the cumulative minerals on the bottom of the magma chamber and their further sorting by specific gravity due to convection currents. Cryptic layering is firstly discovered in the Anagram gabbroids and is explained by the processes of crystallization differentiation. The latter caused the accumulation of the most calcium plagioclases and the most magnesian mafic minerals in the layered gabbroids forming the bottom part of the intrusion. The present subvertical position of layering is explained by tectonic deformation that resulted in the tilting of the investigated section of the Anagram gabbroid intrusion. This confirmed by the studying of magnetic texture of the gabbroids (by the anisotropy of magnetic susceptibility data).
{"title":"The Petrology of Gabbroids of the Anagram Islands (Wilhelm Archipelago, West Antarctica)","authors":"O. Mytrokhyn, V. Bakhmutov, A. Aleksieienko, T. Mytrokhina","doi":"10.15407/mineraljournal.42.04.069","DOIUrl":"https://doi.org/10.15407/mineraljournal.42.04.069","url":null,"abstract":"The Anagram Islands are located near the Graham Coast of West Antarctica not far from the Ukrainian Antarctic Station \"Akademik Vernadsky\". Gabbroids that are probably Cretaceous in age predominate in the geological structure of the Anagram Islands. New data on the mode of occurrence of the Anagram gabbroids and their layering were obtained during the seasonal field works of the Ukrainian Antarctic Expeditions in 2017, 2019-2020 years. Samples of the gabbroids were examined by optical microscopy, electron microscopy and microprobe analysis as well as by measuring of anisotropy of magnetic susceptibility of rocks. The goal of the research was to clarify the geological position and petrographic features of the Anagram gabbroids, to determine the typomorphic features of rock-forming minerals, and to clarify the origin of the layering in gabbroids. It was determined that the bottom part of a large layered gabbroid intrusion is fragmentarily exposed on the Anagram Islands. The continuation of the intrusion is expected in the northeastern and southeastern directions. It was established that primary magmatic textures and mineral composition are preserved in the gabbroids despite the development of metamorphic amphibolization. The gabbroids show typical cumulative textures of magmatic origin. The main cumulative phases are plagioclase (An70-95), clinopyroxene (Wo41-49En34-47), orthopyroxene (Wo2-4En49-71), olivine (Fo67-69), Ti-magnetite and ilmenite. It is proved that the fine rhythmic-gradational layering in the gabbroids was formed by gravitational precipitation of the cumulative minerals on the bottom of the magma chamber and their further sorting by specific gravity due to convection currents. Cryptic layering is firstly discovered in the Anagram gabbroids and is explained by the processes of crystallization differentiation. The latter caused the accumulation of the most calcium plagioclases and the most magnesian mafic minerals in the layered gabbroids forming the bottom part of the intrusion. The present subvertical position of layering is explained by tectonic deformation that resulted in the tilting of the investigated section of the Anagram gabbroid intrusion. This confirmed by the studying of magnetic texture of the gabbroids (by the anisotropy of magnetic susceptibility data).","PeriodicalId":53834,"journal":{"name":"Mineralogical Journal-Ukraine","volume":"42 1","pages":"69-83"},"PeriodicalIF":0.2,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67125903","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2020-01-01DOI: 10.15407/mineraljournal.42.01.049
O. Dubyna, S. Kryvdik, O. Vyshnevskyi
O.V. dubyna, DrSc (Geology), Ass. prof. M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of ukraine 34, Acad. Palladin Ave., kyiv, ukraine, 03142 Taras Shevchenko National university of kyiv, Institute of Geology Educational-scientific institute "Institute of Geology" 90, Vasylkivska Str., kyiv, ukraine, 03022 E-mail: dubyna_a@ukr.net http://orcid.org/0000-0002-6003-4873 S.G. Kryvdik, DrSc (Geology & Mineralogy), Prof., Head of Department M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of ukraine 34, Acad. Palladin Ave., kyiv, ukraine, 03142 E-mail: kryvdik@ukr.net http://orcid.org/0000-0002-8356-1115 O.A. Vyshnevskyi, PhD (Geology & Mineralogy), Senior Research Fellow, Leading Researcher M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of ukraine 34, Acad. Palladin Ave., kyiv, ukraine, 03142 E-mail: vyshnevskyy@i.ua Researcher ID: I-9996-2018
{"title":"MINERALOGICAL AND PETROLOGICAL PECULIARITIES OF GRORUDITES OF EASTERN AZOV AREA (UKRAINE)","authors":"O. Dubyna, S. Kryvdik, O. Vyshnevskyi","doi":"10.15407/mineraljournal.42.01.049","DOIUrl":"https://doi.org/10.15407/mineraljournal.42.01.049","url":null,"abstract":"O.V. dubyna, DrSc (Geology), Ass. prof. M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of ukraine 34, Acad. Palladin Ave., kyiv, ukraine, 03142 Taras Shevchenko National university of kyiv, Institute of Geology Educational-scientific institute \"Institute of Geology\" 90, Vasylkivska Str., kyiv, ukraine, 03022 E-mail: dubyna_a@ukr.net http://orcid.org/0000-0002-6003-4873 S.G. Kryvdik, DrSc (Geology & Mineralogy), Prof., Head of Department M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of ukraine 34, Acad. Palladin Ave., kyiv, ukraine, 03142 E-mail: kryvdik@ukr.net http://orcid.org/0000-0002-8356-1115 O.A. Vyshnevskyi, PhD (Geology & Mineralogy), Senior Research Fellow, Leading Researcher M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of ukraine 34, Acad. Palladin Ave., kyiv, ukraine, 03142 E-mail: vyshnevskyy@i.ua Researcher ID: I-9996-2018","PeriodicalId":53834,"journal":{"name":"Mineralogical Journal-Ukraine","volume":"1 1","pages":""},"PeriodicalIF":0.2,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67124203","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2020-01-01DOI: 10.15407/mineraljournal.42.04.104
V. Yemelianov, Ye.I. Nasiedkin, A. V. Sachko, I. Kuraieva, T. Kоshliakova
The results of long-term observations on the geochemical peculiarities of technogenic lead distribution in atmospheric aerosol of Zaporizhia, as well as in soils, bottom sediments, suspended matter from Dnipro river and substance from wet gas filters of open-hearth furnaces PJSC Zaporizhstal are presented. The actual material was obtained on the basis of comprehensive field monitoring during 2015-2019. Simultaneous involvement of data on hydrometeorological conditions (seasonality, precipitation, wind speeds, directions and duration) in the study area provided a integral approach to the processing and generalization of research results. A number of peculiarities of sedimentary substance distribution in air, interrelations of its anthropogenic and natural components are defined. Correlations were revealed between lead concentrations changes and aeolian mineral component distribution, seasonality, and a number of other factors. The highest concentration of lead was found in solid aerosol particles accumulated by the sedimentary trap at the monitoring site. It was revealed that the average concentration of investigated element in river suspension of Dnipro exceeds significantly background values, and for soils exceeds more than 3.5 times the permissible norms. At the same time, the fixed form of lead in atmospheric aerosol, in contrast to other environmental objects, loses its domination, giving the way to easily soluble forms, so the evidence of environmental hazard. Monitoring of seasonal patterns of the element distribution in the city air showed excess concentrations in the cold period of the year, which, according to the authors, is due to both meteorological conditions and redistribution of natural and anthropogenic factors that serve the driving force in processes of arriving and conversion of lead in atmosphere during different seasons of the year.
{"title":"Lead Distribution in Ground-Level Atmospheric Aerosol of Zaporizhia City","authors":"V. Yemelianov, Ye.I. Nasiedkin, A. V. Sachko, I. Kuraieva, T. Kоshliakova","doi":"10.15407/mineraljournal.42.04.104","DOIUrl":"https://doi.org/10.15407/mineraljournal.42.04.104","url":null,"abstract":"The results of long-term observations on the geochemical peculiarities of technogenic lead distribution in atmospheric aerosol of Zaporizhia, as well as in soils, bottom sediments, suspended matter from Dnipro river and substance from wet gas filters of open-hearth furnaces PJSC Zaporizhstal are presented. The actual material was obtained on the basis of comprehensive field monitoring during 2015-2019. Simultaneous involvement of data on hydrometeorological conditions (seasonality, precipitation, wind speeds, directions and duration) in the study area provided a integral approach to the processing and generalization of research results. A number of peculiarities of sedimentary substance distribution in air, interrelations of its anthropogenic and natural components are defined. Correlations were revealed between lead concentrations changes and aeolian mineral component distribution, seasonality, and a number of other factors. The highest concentration of lead was found in solid aerosol particles accumulated by the sedimentary trap at the monitoring site. It was revealed that the average concentration of investigated element in river suspension of Dnipro exceeds significantly background values, and for soils exceeds more than 3.5 times the permissible norms. At the same time, the fixed form of lead in atmospheric aerosol, in contrast to other environmental objects, loses its domination, giving the way to easily soluble forms, so the evidence of environmental hazard. Monitoring of seasonal patterns of the element distribution in the city air showed excess concentrations in the cold period of the year, which, according to the authors, is due to both meteorological conditions and redistribution of natural and anthropogenic factors that serve the driving force in processes of arriving and conversion of lead in atmosphere during different seasons of the year.","PeriodicalId":53834,"journal":{"name":"Mineralogical Journal-Ukraine","volume":"42 1","pages":"104-115"},"PeriodicalIF":0.2,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67125472","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2020-01-01DOI: 10.15407/mineraljournal.42.03.069
I. Nikolaev, E. Sheremet, S. Kryvdik, S. Strekozov, L. Sietaia
{"title":"Prediction of Ore Occurrences in South-Eastern Ukraine","authors":"I. Nikolaev, E. Sheremet, S. Kryvdik, S. Strekozov, L. Sietaia","doi":"10.15407/mineraljournal.42.03.069","DOIUrl":"https://doi.org/10.15407/mineraljournal.42.03.069","url":null,"abstract":"","PeriodicalId":53834,"journal":{"name":"Mineralogical Journal-Ukraine","volume":"42 1","pages":"69-86"},"PeriodicalIF":0.2,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67125818","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2020-01-01DOI: 10.15407/mineraljournal.42.01.036
H. Kulchytska, D. Chernysh, I. M. Herasymets
{"title":"MINERALOGICAL AND THERMOBAROMETRIC MELT LIQUATION SINGS IN HYPERSOLVUS SYENITES (UKRAINIAN SHIELD)","authors":"H. Kulchytska, D. Chernysh, I. M. Herasymets","doi":"10.15407/mineraljournal.42.01.036","DOIUrl":"https://doi.org/10.15407/mineraljournal.42.01.036","url":null,"abstract":"","PeriodicalId":53834,"journal":{"name":"Mineralogical Journal-Ukraine","volume":"42 1","pages":"36-48"},"PeriodicalIF":0.2,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67124169","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2020-01-01DOI: 10.15407/mineraljournal.42.02.020
K. Repina, T. Volkova, V. Zagnitko, V. Moroz, L. Proskurka
{"title":"Mineral Formation in Carbonate Rocks From the Novotroitsk Deposit, the Zone Between the Donbas and the Priazov Megablock","authors":"K. Repina, T. Volkova, V. Zagnitko, V. Moroz, L. Proskurka","doi":"10.15407/mineraljournal.42.02.020","DOIUrl":"https://doi.org/10.15407/mineraljournal.42.02.020","url":null,"abstract":"","PeriodicalId":53834,"journal":{"name":"Mineralogical Journal-Ukraine","volume":"42 1","pages":"20-31"},"PeriodicalIF":0.2,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67124451","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2020-01-01DOI: 10.15407/mineraljournal.42.04.060
Y. Malkova, V. Bobkov, V. Dolin
The article deals with the peculiarities of the chemical composition formation of brines in the Dombrovsky quarry, primarily due to the dissolution of potash ore minerals and host rocks in water coming from the pebble horizon and atmospheric precipitation. The solubility of the ore body minerals has been studied, and it ranges from 333 to 502 g∙dm–3. The boundary conditions for the formation of a saturated salt solution were determined. The estimated concentration of saturated potash ore solution under normal conditions is 426 g∙dm–3. The mechanism of dissolution is considered from the standpoint of D.I. Mendeleev's chemical theory of solutions. The temporary dynamics of minerals dissolution of the ore body is studied experimentally. The parameters of kinetic-diffusion process are calculated. The rate of the dissolution process, which occurs in the kinetic region, significantly exceeds the rate of concentration diffusion of hydrated ions: from 5 to 400 times depending on the mineral composition of salts. Theoretically from the point of view of multistage process kinetics and experimentally in laboratory conditions it is proved that the process that determines the formation of the chemical composition of brines (the slowest stage) is the concentration diffusion of hydrated ions Na+, K+, Cl–. They enter the liquid phase due to the minerals dissolution of the ore body and host rocks of soil and sides of the quarry, in the direction of overcoming the concentration difference - from the lower layers of the brine to its surface. This conclusion is confirmed by the ratio of weight coefficients а1 and а2. The contribution of the process of the main minerals dissolution of the ore body to the chemical composition formation of the solution is significantly less than the concentration diffusion process.
{"title":"Modeling the Kinetics of Saline Minerals Dissolution in Dombrovsky Quarry at the Kalush-Golinsky Potassium Salts Deposit","authors":"Y. Malkova, V. Bobkov, V. Dolin","doi":"10.15407/mineraljournal.42.04.060","DOIUrl":"https://doi.org/10.15407/mineraljournal.42.04.060","url":null,"abstract":"The article deals with the peculiarities of the chemical composition formation of brines in the Dombrovsky quarry, primarily due to the dissolution of potash ore minerals and host rocks in water coming from the pebble horizon and atmospheric precipitation. The solubility of the ore body minerals has been studied, and it ranges from 333 to 502 g∙dm–3. The boundary conditions for the formation of a saturated salt solution were determined. The estimated concentration of saturated potash ore solution under normal conditions is 426 g∙dm–3. The mechanism of dissolution is considered from the standpoint of D.I. Mendeleev's chemical theory of solutions. The temporary dynamics of minerals dissolution of the ore body is studied experimentally. The parameters of kinetic-diffusion process are calculated. The rate of the dissolution process, which occurs in the kinetic region, significantly exceeds the rate of concentration diffusion of hydrated ions: from 5 to 400 times depending on the mineral composition of salts. Theoretically from the point of view of multistage process kinetics and experimentally in laboratory conditions it is proved that the process that determines the formation of the chemical composition of brines (the slowest stage) is the concentration diffusion of hydrated ions Na+, K+, Cl–. They enter the liquid phase due to the minerals dissolution of the ore body and host rocks of soil and sides of the quarry, in the direction of overcoming the concentration difference - from the lower layers of the brine to its surface. This conclusion is confirmed by the ratio of weight coefficients а1 and а2. The contribution of the process of the main minerals dissolution of the ore body to the chemical composition formation of the solution is significantly less than the concentration diffusion process.","PeriodicalId":53834,"journal":{"name":"Mineralogical Journal-Ukraine","volume":"42 1","pages":"60-68"},"PeriodicalIF":0.2,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67125757","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2020-01-01DOI: 10.15407/mineraljournal.42.03.050
L. Stepanyuk, L. Shumlyanskyy, V. Gatsenko, I. M. Lisna, T. Dovbush, S. Wilde, A. Nemchin, B. Bagiński, O. Bilan
{"title":"The U-Pb Zircon Geochronology (LA-ICP-MS) of Geological Processes in Granulites of Middle Bouh Area. Article 1. Rock association in the Kosharo-Oleksandrivka open pit","authors":"L. Stepanyuk, L. Shumlyanskyy, V. Gatsenko, I. M. Lisna, T. Dovbush, S. Wilde, A. Nemchin, B. Bagiński, O. Bilan","doi":"10.15407/mineraljournal.42.03.050","DOIUrl":"https://doi.org/10.15407/mineraljournal.42.03.050","url":null,"abstract":"","PeriodicalId":53834,"journal":{"name":"Mineralogical Journal-Ukraine","volume":"42 1","pages":"50-68"},"PeriodicalIF":0.2,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67125795","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2020-01-01DOI: 10.15407/mineraljournal.42.04.033
O. Chepizhko, V. Yanko, V. M. Kadurin, I. Naumko, S. Shatalin
For the first time the importance of mineralogical and lithological-petrographical ranks in the line of geological information ranks is substantiated for implementation of long-term forecasts, standard and non-standard approaches to research of physical and geochemical parameters as a basis of creation of complex system of forecast criteria and prospecting indicators of hydrocarbons within the sedimentary cover of Black sea based on the theory of global fluid-flows derivation. These criteria have different sensitivity to the object (hydrocarbon deposits) and are therefore ranked. The ranking determined the following parameters: 1) seismic data within the object, obtained by the method of deep seismic sounding, RWM SDP; 2) parameters of tectono-geodynamic structures; 3) the main characteristics of sedimentary cover and bedrock; 4) geochemical characteristics; 5) parameters of mineral complexes and fluid inclusions in mineral neoformations; 6) the value of the distribution of meiobenthos. Based on modern views of oil and gas geology, structural-tectonic and lithological-facies criteria are among the main ones. The study of the mineralogical component of sediments is made with using mineralogical, thermobarogeochemical and X-ray spectral methods. Fixation of anomalies of fluid flow at the bottom of the Black Sea as to the distribution of abiotic parameters in order to assess the prospects of oil and gas is determined by structural and tectonic features and high permeability of fluid flow; parameters of mineral complexes (minerals, facies) and genetic connections; heterogeneity of geochemical characteristics of bottom sediments; the presence of hydrocarbon inclusions in authigenic minerals of bottom sediments.
{"title":"Significance of Mineralogical and Lithologic-Petrographical Rank in the Ranking of Geological Information","authors":"O. Chepizhko, V. Yanko, V. M. Kadurin, I. Naumko, S. Shatalin","doi":"10.15407/mineraljournal.42.04.033","DOIUrl":"https://doi.org/10.15407/mineraljournal.42.04.033","url":null,"abstract":"For the first time the importance of mineralogical and lithological-petrographical ranks in the line of geological information ranks is substantiated for implementation of long-term forecasts, standard and non-standard approaches to research of physical and geochemical parameters as a basis of creation of complex system of forecast criteria and prospecting indicators of hydrocarbons within the sedimentary cover of Black sea based on the theory of global fluid-flows derivation. These criteria have different sensitivity to the object (hydrocarbon deposits) and are therefore ranked. The ranking determined the following parameters: 1) seismic data within the object, obtained by the method of deep seismic sounding, RWM SDP; 2) parameters of tectono-geodynamic structures; 3) the main characteristics of sedimentary cover and bedrock; 4) geochemical characteristics; 5) parameters of mineral complexes and fluid inclusions in mineral neoformations; 6) the value of the distribution of meiobenthos. Based on modern views of oil and gas geology, structural-tectonic and lithological-facies criteria are among the main ones. The study of the mineralogical component of sediments is made with using mineralogical, thermobarogeochemical and X-ray spectral methods. Fixation of anomalies of fluid flow at the bottom of the Black Sea as to the distribution of abiotic parameters in order to assess the prospects of oil and gas is determined by structural and tectonic features and high permeability of fluid flow; parameters of mineral complexes (minerals, facies) and genetic connections; heterogeneity of geochemical characteristics of bottom sediments; the presence of hydrocarbon inclusions in authigenic minerals of bottom sediments.","PeriodicalId":53834,"journal":{"name":"Mineralogical Journal-Ukraine","volume":"42 1","pages":"33-49"},"PeriodicalIF":0.2,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67125675","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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