Graviseismic structure of the earth’s crust and its five-oceanic geostrophe
Background. The priority positions of Russian geology and geophysics have been reliably supported by large volumes of mineral resources of Eurasian proto-ocean/EAO from ancient Arctic to Middle East. This ocean bordered on all its sides by four other proto-oceans that were opened step-by-step to dif...
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Sergo Ordzhonikidze Russian State University for Geological Prospecting
2025-07-01
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| Series: | Известия высших учебных заведений: Геология и разведка |
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| Online Access: | https://www.geology-mgri.ru/jour/article/view/1149 |
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| author | A. F. Glebov |
| author_facet | A. F. Glebov |
| author_sort | A. F. Glebov |
| collection | DOAJ |
| description | Background. The priority positions of Russian geology and geophysics have been reliably supported by large volumes of mineral resources of Eurasian proto-ocean/EAO from ancient Arctic to Middle East. This ocean bordered on all its sides by four other proto-oceans that were opened step-by-step to different sizes between Gondwana, Europe and Asia with Siberia (G-E-A).Aim. Graviseismic modeling of the Earth’s crust as a basis for RTOE-determination of four tectonic (rifto-, thalasso-, oro-, & epeiro-genic) regimes and a five-oceanic geostrophe of the Earth with two circumpolar and three intercontinental oceans.Materials and methods. Collection and integration of actual geological and geophysical data on the world’s petroleum and mineragenic provinces to carry out a four-segment (RT-TO-OE-ER) zoning of the Earth’s crust and a sequence stratification of four system tracts (UST-MST-DST-LST formations) taking into account global fluctuations (up, max, down, low/min) of the sea level.Results. Graviseismic identification of eight geostrophic plates of the modern Earth’s crust with its four-segment zoning and seismo-geological stratification into 12 global sequences.Conclusion. A new graviseismic concept of a five-oceanic geostrophe of the Earth’s crust has been developed, which is capable of elucidating both past and future stages of the tectono-stratigraphic evolution of sedimentary provinces since the origin of the World Ocean. |
| format | Article |
| id | doaj-art-24efbd2b277047428fa690bba9bda478 |
| institution | DOAJ |
| issn | 0016-7762 2618-8708 |
| language | Russian |
| publishDate | 2025-07-01 |
| publisher | Sergo Ordzhonikidze Russian State University for Geological Prospecting |
| record_format | Article |
| series | Известия высших учебных заведений: Геология и разведка |
| spelling | doaj-art-24efbd2b277047428fa690bba9bda4782025-08-20T03:19:12ZrusSergo Ordzhonikidze Russian State University for Geological ProspectingИзвестия высших учебных заведений: Геология и разведка0016-77622618-87082025-07-01672607510.32454/0016-7762-2025-67-2-60-75653Graviseismic structure of the earth’s crust and its five-oceanic geostropheA. F. Glebov0Intergovernmental Oil &Gas Company “SouyzNefteGas”Background. The priority positions of Russian geology and geophysics have been reliably supported by large volumes of mineral resources of Eurasian proto-ocean/EAO from ancient Arctic to Middle East. This ocean bordered on all its sides by four other proto-oceans that were opened step-by-step to different sizes between Gondwana, Europe and Asia with Siberia (G-E-A).Aim. Graviseismic modeling of the Earth’s crust as a basis for RTOE-determination of four tectonic (rifto-, thalasso-, oro-, & epeiro-genic) regimes and a five-oceanic geostrophe of the Earth with two circumpolar and three intercontinental oceans.Materials and methods. Collection and integration of actual geological and geophysical data on the world’s petroleum and mineragenic provinces to carry out a four-segment (RT-TO-OE-ER) zoning of the Earth’s crust and a sequence stratification of four system tracts (UST-MST-DST-LST formations) taking into account global fluctuations (up, max, down, low/min) of the sea level.Results. Graviseismic identification of eight geostrophic plates of the modern Earth’s crust with its four-segment zoning and seismo-geological stratification into 12 global sequences.Conclusion. A new graviseismic concept of a five-oceanic geostrophe of the Earth’s crust has been developed, which is capable of elucidating both past and future stages of the tectono-stratigraphic evolution of sedimentary provinces since the origin of the World Ocean.https://www.geology-mgri.ru/jour/article/view/1149earth’s crustgravity and magmatismbouguer anomalies and moho depthsgeoid and seismicityplates of geostrophic subsidence or upliftlithospheric segments and their epicentral regionsquasi-equilibrium and saddle-shear borderlinestectonic regimes and geodynamic settingssedimentary formations and petroleum sequences |
| spellingShingle | A. F. Glebov Graviseismic structure of the earth’s crust and its five-oceanic geostrophe Известия высших учебных заведений: Геология и разведка earth’s crust gravity and magmatism bouguer anomalies and moho depths geoid and seismicity plates of geostrophic subsidence or uplift lithospheric segments and their epicentral regions quasi-equilibrium and saddle-shear borderlines tectonic regimes and geodynamic settings sedimentary formations and petroleum sequences |
| title | Graviseismic structure of the earth’s crust and its five-oceanic geostrophe |
| title_full | Graviseismic structure of the earth’s crust and its five-oceanic geostrophe |
| title_fullStr | Graviseismic structure of the earth’s crust and its five-oceanic geostrophe |
| title_full_unstemmed | Graviseismic structure of the earth’s crust and its five-oceanic geostrophe |
| title_short | Graviseismic structure of the earth’s crust and its five-oceanic geostrophe |
| title_sort | graviseismic structure of the earth s crust and its five oceanic geostrophe |
| topic | earth’s crust gravity and magmatism bouguer anomalies and moho depths geoid and seismicity plates of geostrophic subsidence or uplift lithospheric segments and their epicentral regions quasi-equilibrium and saddle-shear borderlines tectonic regimes and geodynamic settings sedimentary formations and petroleum sequences |
| url | https://www.geology-mgri.ru/jour/article/view/1149 |
| work_keys_str_mv | AT afglebov graviseismicstructureoftheearthscrustanditsfiveoceanicgeostrophe |