Pub Date : 2021-01-01DOI: 10.15407/gpimo2021.04.052
M. Shatalov
Among geologists of the 20—30 years of the twentieth century. the leading place in Ukraine was occupied by the repressed in 1937, professor Roman Romanovych Vyrzhykivsky (1891—1937). At the Kiev University of St. Vladimir, he was a very capable student of N.I. Andrusov and the famous petrographer and mineralogist, professor, later academician V.I. Luchitsky. In the history of geological science, R.R. Vyrzhykivsky entered as a researcher of the Black Sea region, and the south-west of the European part of the USSR (Ukraine, Moldova), as well as a talented organizer of geological work, a brilliant surveyor geologist, tectonist and an outstanding hydrogeologist. The scientist was the head of geological survey work in Transnistria and prepared for printing the first geological map of 10 versts scale — «Transnistria» (Dniester region). Later, this map became the basis for prospecting and exploration of mineral deposits in Transnistria. In the studied region, he first discovered numerous deposits of phosphorites, cement raw materials, kaolin, flint, building sands, sandstones, tripoli, lithographic stone and underground drinking water. At the same time, the young scientist described for the first time a unique ridge of reef limestones of Middle Sarmatian age, which he traced in the meridional direction from the lower reaches of the river Kamenka along its left bank to the north, in Podillia. In the Shargorod region of Transnistria (Dniester region), the scientist found Paleogene marine deposits, and he identified the Podolsk stage in the Miocene layers of Podolia. In a number of scientific works of Roman Romanovich, data are presented in the field of fault-block tectonics and neotectonic movements of Transnistria and the Black Sea region. R.R. Vyrzhykivsky also considered the issue of modern transgressions of the Black Sea in the most complete way. This work of the scientist was one of the first evidence of the manifestation of the latest tectonic movements in the region of the Northern Black Sea region and the Black Sea. R.R. Vyrzhykivsky rightfully belongs to the galaxy of the greatest scientists—hydrogeologists of Ukraine and Moldova. In particular, he laid the foundations for the hydrogeological zoning of the territory of Moldova for the first time. Within Moldova, he identified the Middle Sarmatian, Cretaceous and Silurian water-saturated horizons. Merits of R.R. Vyrzhykivsky in the field of hydrogeological problems of Ukraine can hardly be overestimated. He made a huge practical contribution to the water supply of large industrial cities and agglomerations of the country. In 1932 R.R. Vyrzhykivsky published the monograph «Hydrogeology» in Ukrainian, which played a huge role in the training of national hydrogeologists. In it, he for the first time presented the results of the hydrogeological zoning of the territory of Ukraine. It is important that the hydrogeological zoning scheme, with minor changes, is still being used by the hydrogeologists of o
{"title":"PROFESSOR ROMAN ROMANOVYCH VYRZHYKIVSKY. To the 130th anniversary of the birthday","authors":"M. Shatalov","doi":"10.15407/gpimo2021.04.052","DOIUrl":"https://doi.org/10.15407/gpimo2021.04.052","url":null,"abstract":"Among geologists of the 20—30 years of the twentieth century. the leading place in Ukraine was occupied by the repressed in 1937, professor Roman Romanovych Vyrzhykivsky (1891—1937). At the Kiev University of St. Vladimir, he was a very capable student of N.I. Andrusov and the famous petrographer and mineralogist, professor, later academician V.I. Luchitsky. In the history of geological science, R.R. Vyrzhykivsky entered as a researcher of the Black Sea region, and the south-west of the European part of the USSR (Ukraine, Moldova), as well as a talented organizer of geological work, a brilliant surveyor geologist, tectonist and an outstanding hydrogeologist. The scientist was the head of geological survey work in Transnistria and prepared for printing the first geological map of 10 versts scale — «Transnistria» (Dniester region). Later, this map became the basis for prospecting and exploration of mineral deposits in Transnistria. In the studied region, he first discovered numerous deposits of phosphorites, cement raw materials, kaolin, flint, building sands, sandstones, tripoli, lithographic stone and underground drinking water. At the same time, the young scientist described for the first time a unique ridge of reef limestones of Middle Sarmatian age, which he traced in the meridional direction from the lower reaches of the river Kamenka along its left bank to the north, in Podillia. In the Shargorod region of Transnistria (Dniester region), the scientist found Paleogene marine deposits, and he identified the Podolsk stage in the Miocene layers of Podolia. In a number of scientific works of Roman Romanovich, data are presented in the field of fault-block tectonics and neotectonic movements of Transnistria and the Black Sea region. R.R. Vyrzhykivsky also considered the issue of modern transgressions of the Black Sea in the most complete way. This work of the scientist was one of the first evidence of the manifestation of the latest tectonic movements in the region of the Northern Black Sea region and the Black Sea. R.R. Vyrzhykivsky rightfully belongs to the galaxy of the greatest scientists—hydrogeologists of Ukraine and Moldova. In particular, he laid the foundations for the hydrogeological zoning of the territory of Moldova for the first time. Within Moldova, he identified the Middle Sarmatian, Cretaceous and Silurian water-saturated horizons. Merits of R.R. Vyrzhykivsky in the field of hydrogeological problems of Ukraine can hardly be overestimated. He made a huge practical contribution to the water supply of large industrial cities and agglomerations of the country. In 1932 R.R. Vyrzhykivsky published the monograph «Hydrogeology» in Ukrainian, which played a huge role in the training of national hydrogeologists. In it, he for the first time presented the results of the hydrogeological zoning of the territory of Ukraine. It is important that the hydrogeological zoning scheme, with minor changes, is still being used by the hydrogeologists of o","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67115071","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/gpimo2020.01.069
{"title":"A pioneer in marine scientific geological research in the areas of the Black and Azov Seas — Ye.F. Shnyukov","authors":"","doi":"10.15407/gpimo2020.01.069","DOIUrl":"https://doi.org/10.15407/gpimo2020.01.069","url":null,"abstract":"","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67114753","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/gpimo2020.03.003
S. Pletnev, T. E. Sedysheva
Fe-Mn crusts play an important role in marine mineral deposit research because of their widespread occurrence and high concentrations of valuable and rare metals. Most Fe-Mn crust deposits occur on the tens of thousands of seamounts found in the ocean. Data on the structure, texture, composition, age, and deposit characteristics will help define which factors are key for the creation of mineral accumulation and which combination of factors leads to the formation of potentially economic concentrations of metals. In this paper, we address the structure and characteristics of the oldest Fe-Mn crust stratigraphic sections (Late Cretaceous and Paleocene) collected from the Magellan seamounts. A complete section of the crusts on the Magellan Seamounts includes four layers, each 2—4 cm thickness: the Late Paleocene (?) Early Eocene layer I 1, the Mid Late Eocene layer I—2, the Miocene layer II and the Quaternary layer III. In some cases, the main CMC section is underlain by relict layers. The chemical and mineral composition of the layers was determined both by X-ray diffraction and precision methods; concentrations of the main ore components and phosphorus were determined by the methods of classical chemistry. The age of 12 samples was determined, the mineral composition of four, the chemical composition of 22 samples. The results of the relict layers analysis allow to distinguish two groups of samples among them. Among the relict layers, two age ranges are established — the second half of Late Cretaceous (R1) and the first half of Paleocene (R2). High concentrations of barium, lithium, gallium, and zinc suggest that hydrothermal sources could be the source of the material. But not through direct delivery, but via the phase of transfer of sea bottom water. Thus, the analysis of lithological and geochemical parameters and fossil fauna of foraminifera in the relict layers of the Magellan Seamounts ore section indicates two stages of their formation: Late Campan Maastricht and Early Middle Paleocene. The discreteness of the formation of relict layers in time once again proves that the sharply changing environmental conditions controlled the growth of the CMC ore section.
{"title":"The early stages of ferromanganese ore genesis on the guyots of the Magellan Seamounts (The Pacific Ocean)","authors":"S. Pletnev, T. E. Sedysheva","doi":"10.15407/gpimo2020.03.003","DOIUrl":"https://doi.org/10.15407/gpimo2020.03.003","url":null,"abstract":"Fe-Mn crusts play an important role in marine mineral deposit research because of their widespread occurrence and high concentrations of valuable and rare metals. Most Fe-Mn crust deposits occur on the tens of thousands of seamounts found in the ocean. Data on the structure, texture, composition, age, and deposit characteristics will help define which factors are key for the creation of mineral accumulation and which combination of factors leads to the formation of potentially economic concentrations of metals. In this paper, we address the structure and characteristics of the oldest Fe-Mn crust stratigraphic sections (Late Cretaceous and Paleocene) collected from the Magellan seamounts. A complete section of the crusts on the Magellan Seamounts includes four layers, each 2—4 cm thickness: the Late Paleocene (?) Early Eocene layer I 1, the Mid Late Eocene layer I—2, the Miocene layer II and the Quaternary layer III. In some cases, the main CMC section is underlain by relict layers. The chemical and mineral composition of the layers was determined both by X-ray diffraction and precision methods; concentrations of the main ore components and phosphorus were determined by the methods of classical chemistry. The age of 12 samples was determined, the mineral composition of four, the chemical composition of 22 samples. The results of the relict layers analysis allow to distinguish two groups of samples among them. Among the relict layers, two age ranges are established — the second half of Late Cretaceous (R1) and the first half of Paleocene (R2). High concentrations of barium, lithium, gallium, and zinc suggest that hydrothermal sources could be the source of the material. But not through direct delivery, but via the phase of transfer of sea bottom water. Thus, the analysis of lithological and geochemical parameters and fossil fauna of foraminifera in the relict layers of the Magellan Seamounts ore section indicates two stages of their formation: Late Campan Maastricht and Early Middle Paleocene. The discreteness of the formation of relict layers in time once again proves that the sharply changing environmental conditions controlled the growth of the CMC ore section.","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67114764","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/gpimo2020.04.003
A. Sobisevich
The success of recently developed geological and geophysical methods and technologies for monitoring of mud volcanoes in the Kerch-Taman region is eventually based on the fundamental scientific results accumulated at the turn of the century under the overall leadership of the Academician E.F. Shnyukov. The results of geological and geophysical studies of the Mount Karabetov mud volcano (Taman Peninsula) featuring the passive seismoacoustic sounding method are presented. New data on the spatial configuration of subvertical fluid-saturated structures associated with the volcano's feeding system were obtained. Subsequent common interpretation of the geophysical data and the results of the structural-geomorphologic observations allowed one to formulate a consistent hypothesis on the possible deep mechanism of mud volcanic activity responsible for the mostly paroxysmal nature of eruptions of the Mount Karabetov.
{"title":"THE EARLY STAGES OF FERROMANGANESE ORE GENESIS ON THE GUYOTS OF THE MAGELLAN SEAMOUNTS (THE PACIFIC OCEAN)","authors":"A. Sobisevich","doi":"10.15407/gpimo2020.04.003","DOIUrl":"https://doi.org/10.15407/gpimo2020.04.003","url":null,"abstract":"The success of recently developed geological and geophysical methods and technologies for monitoring of mud volcanoes in the Kerch-Taman region is eventually based on the fundamental scientific results accumulated at the turn of the century under the overall leadership of the Academician E.F. Shnyukov. The results of geological and geophysical studies of the Mount Karabetov mud volcano (Taman Peninsula) featuring the passive seismoacoustic sounding method are presented. New data on the spatial configuration of subvertical fluid-saturated structures associated with the volcano's feeding system were obtained. Subsequent common interpretation of the geophysical data and the results of the structural-geomorphologic observations allowed one to formulate a consistent hypothesis on the possible deep mechanism of mud volcanic activity responsible for the mostly paroxysmal nature of eruptions of the Mount Karabetov.","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":"35 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2020-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67114810","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 : 2019-03-01DOI: 10.15407/GPIMO2019.01.087
I. Lomakin, V. Kochelab
{"title":"THIN AND DISPERSED GOLD PLACER OF THE SEDIMENTARY COVER OF THE NORTHWESTERN BLACK SEA COAST. PROBLEMS AND PROSPECTS","authors":"I. Lomakin, V. Kochelab","doi":"10.15407/GPIMO2019.01.087","DOIUrl":"https://doi.org/10.15407/GPIMO2019.01.087","url":null,"abstract":"","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45579541","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 : 2019-03-01DOI: 10.15407/gpimo2019.01.032
M. Pavlyuk, M. Yakovenko
{"title":"OIL- AND GAS-BEARING POTENTIAL SEA AREAS OF THE EAST EUROPEAN PLATFORM","authors":"M. Pavlyuk, M. Yakovenko","doi":"10.15407/gpimo2019.01.032","DOIUrl":"https://doi.org/10.15407/gpimo2019.01.032","url":null,"abstract":"","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42640810","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 : 2019-03-01DOI: 10.15407/GPIMO2019.01.115
S. Yesypovych
{"title":"ANTARCTICA IS THE SOUTHERN GEOGRAPHICAL AREA OF THE EARTH AS A GEODYNAMIC CENTER OF FORMATION OF THE PRIMARY CRUST OF THE PLANET","authors":"S. Yesypovych","doi":"10.15407/GPIMO2019.01.115","DOIUrl":"https://doi.org/10.15407/GPIMO2019.01.115","url":null,"abstract":"","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42552944","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 : 2019-03-01DOI: 10.15407/GPIMO2019.01.003
Y. Shnyukov
{"title":"BLACK SEA: THE FUTURE OF THE MINERAL RESOURCE BASE","authors":"Y. Shnyukov","doi":"10.15407/GPIMO2019.01.003","DOIUrl":"https://doi.org/10.15407/GPIMO2019.01.003","url":null,"abstract":"","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"41477471","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 : 2019-03-01DOI: 10.15407/GPIMO2019.01.018
P. Gozhik, V. E. Rokytskyi
{"title":"NEW DATA ON THE DISTRIBUTION OF SEDIMENTS OF THE DANUBE FORMATION","authors":"P. Gozhik, V. E. Rokytskyi","doi":"10.15407/GPIMO2019.01.018","DOIUrl":"https://doi.org/10.15407/GPIMO2019.01.018","url":null,"abstract":"","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"48746970","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 : 2019-03-01DOI: 10.15407/gpimo2019.01.074
Yu.I. Inozemtcev, O. O. Paryshev, Z. V. Krasnozhyna, M. Maslakov
{"title":"MAGNETITE FROM COASTAL DEPOZITS OF BLACK AND AZOV SEAS","authors":"Yu.I. Inozemtcev, O. O. Paryshev, Z. V. Krasnozhyna, M. Maslakov","doi":"10.15407/gpimo2019.01.074","DOIUrl":"https://doi.org/10.15407/gpimo2019.01.074","url":null,"abstract":"","PeriodicalId":33769,"journal":{"name":"Geologiia i poleznye iskopaemye mirovogo okeana","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"41567031","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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