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dc.contributor.author Zhan W.
dc.contributor.author Sun L.
dc.contributor.author Sun Z.
dc.contributor.author Yao Y.
dc.contributor.author Qiu X.
dc.contributor.author Zhu Z.
dc.date.accessioned 2024-09-04T09:55:33Z
dc.date.available 2024-09-04T09:55:33Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=31383822
dc.identifier.citation Acta Geologica Sinica (English Edition), 2006, 80, 4, 491-496
dc.identifier.issn 1000-9515
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/44901
dc.description.abstract Based on the topography, geophysical profiles, gravity and magnetic anomalies, structural characteristics and crustal dynamic environment, the paper illustrates the epoch and diversities of the neotectonic movement in the South China Sea. The traditional point looks the late Tertiary as the beginning of the neotectonic movement in the South China Sea. So as this view, the stratum between early and late Tertiary should be unconformable. But there are no many tectonic events during this period. From middle Miocene to late Miocene there is a stage of peneplanation in the South China Sea and there are many tectonic events in this area, such as stratum unconformable contact, faults, deformation and magmatism. So we think the neotectonic movement in the South China Sea begins in middle Miocene. By contrasting the tectonic event between the middle Miocene to late Miocene in the South China Sea, we can see the neotectonic movement has distinct characteristics in different area.
dc.subject DIVERSITIES
dc.subject NEOTECTONIC MOVEMENT
dc.subject EPOCH
dc.subject SOUTH CHINA SEA
dc.title THE EPOCH AND DIVERSITIES OF NEOTECTONIC MOVEMENT IN THE SOUTH CHINA SEA
dc.type Статья
dc.subject.age Кайнозой::Неоген::Миоцен
dc.subject.age Cenozoic::Neogene::Miocene


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