On the continuity and discreteness of the lithosphere in the problems of dynamic geology

Короновский, Н. В.; Наймарк, А. А.

doi:10.3103/s0145875215010020

Cited by 2 publications

(4 citation statements)

References 7 publications

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“…Таким образом, Мировой океан был сформирован почти полностью к концу кайнозоя. В начале голоцена климат в Арктике был теплый и там росли лиственные леса, бродили стада крупных животных и были поселения людей [21,22]. Но в середине голоцена (6 тыс.…”

Section: рис 5 Cейсмологический разрез по линии татарский пролив -сах...unclassified

“…Formation of Honshu Island during eight tectonic-sedimentation cycles, from Devonian to Neogene [6,12] ский, Гренландский и Норвежский глубокие грабены быстро заполнились водой, тем самым единый прежде мегаконтинент был разделен на два обособленных географических материка -Американский и Евразийско-Африканский [18]. Но вода была теплой, на несколько градусов теплее современной воды [22].…”

Section: рис 5 Cейсмологический разрез по линии татарский пролив -сах...unclassified

“…Это событие произошло, по разным данным [1,22,28], около 6 тыс. лет назад и сохранилось в памяти народов многих стран как «великий потоп».…”

Section: рис 5 Cейсмологический разрез по линии татарский пролив -сах...unclassified

“…Около 4 тыс. лет назад в Арктике наступило новое похолодание [22]. Арктический океан покрылся круглогодичным льдом и стал называться в России Северным Ледовитым океаном.…”

Section: рис 5 Cейсмологический разрез по линии татарский пролив -сах...unclassified

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On the Vertical Growth of the Earth’s Crust in the East Asia Outskirts and Its Flooding by the World Ocean Six Thousand Years Ago

Zhirnov¹

2023

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The relevance of the study is determined by the need of considering the earth’s crust in the East Asia outskirts, as there are various contradictory judgments on its origin. The purpose of the work is to characterize the geological structure of the eastern margin of Asia, supplemented with new data. To solve the problem, it is used numerous geological data and seismic sections of the territory, obtained by means of its detailed studies in the twentieth century, and new data. It is established that the eastern margin of Asia has a three-layered continental structure. Its active vertical geological development took place in the Precambrian (4.5–1.7 billion years ago), when the ancient crystalline foundation was created, partly in the Paleozoic, and most powerfully in the Mesozoic-Cenozoic time, when certain parts of the territory underwent several tectonic-magmatic cycles. During the Neocene-Quaternary period, there intensified vertical tectonic movements, volcanism and seismicity. Six thousand years ago, significant flat parts of the territory were covered by sea waters due to the increase in the level of the World Ocean, with the formation of large grabens in the Arctic and the Asia outskirts. Therefore, there appeared a wide shallow shelf and separate deep seas (3–7 km). In addition to well-established facts on the structure of the Earth's crust, there are also the discussion ideas based on plate tectonics and paleomagnetism –movements of individual tectonic blocks and even individual continents from south to north, by a distance of up to 2 thousand kilometers, and the oceanic crust immersion under the outskirts of Asia.

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Section: рис 5 Cейсмологический разрез по линии татарский пролив -сах...unclassified

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On the Vertical Growth of the Earth’s Crust in the East Asia Outskirts and Its Flooding by the World Ocean Six Thousand Years Ago

Zhirnov¹

2023

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Use of controlled dynamic impacts on hierarchically structured seismically hazardous faults for seismically safe relaxation of shear stresses

Ruzhich

Psakhie

Левина

et al. 2017

AIP Conference Proceedings

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On the continuity and discreteness of the lithosphere in the problems of dynamic geology

Cited by 2 publications

References 7 publications

On the Vertical Growth of the Earth’s Crust in the East Asia Outskirts and Its Flooding by the World Ocean Six Thousand Years Ago

On the Vertical Growth of the Earth’s Crust in the East Asia Outskirts and Its Flooding by the World Ocean Six Thousand Years Ago

Use of controlled dynamic impacts on hierarchically structured seismically hazardous faults for seismically safe relaxation of shear stresses

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