On tectonic movement in the South China Sea during the Cenozoic

LIN Chang-song; CHU Feng-you; GAO Jin-yao; TAN Yong-hua

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LIN Chang-song, CHU Feng-you, GAO Jin-yao, TAN Yong-hua. On tectonic movement in the South China Sea during the Cenozoic[J]. Haiyang Xuebao, 2007, 29(4): 87-96.

Citation:

LIN Chang-song, CHU Feng-you, GAO Jin-yao, TAN Yong-hua. On tectonic movement in the South China Sea during the Cenozoic[J]. Haiyang Xuebao, 2007, 29(4): 87-96.

LIN Chang-song, CHU Feng-you, GAO Jin-yao, TAN Yong-hua. On tectonic movement in the South China Sea during the Cenozoic[J]. Haiyang Xuebao, 2007, 29(4): 87-96.

Citation:

LIN Chang-song, CHU Feng-you, GAO Jin-yao, TAN Yong-hua. On tectonic movement in the South China Sea during the Cenozoic[J]. Haiyang Xuebao, 2007, 29(4): 87-96.

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On tectonic movement in the South China Sea during the Cenozoic

Key Laboratory of Submarine Geosciences of State Oceanic Administration, Hangzhou 310012, China;Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China

Received Date: 2006-07-31
Rev Recd Date: 2006-09-29

Abstract

Abstract

The tectonic movement at the end of Cretacious and the beginning of Cenozoic had opened the Cenozoic phase of poly cyclic tectonic movement,then the whole crust of the South China Sea had been mainly subjected to the regional stress field of tectonic tension,which was characterized by rifting depression.Seven times of regional tectonic movement and sedimentation had been assembled into ageological development history of polycyclic oscillatory.Especially,the tectonic movement was strongly intensified at the end of Cretacious and the beginning of Paleagene,between the Late Eocene and the Mid-Oligocene, during the Mid-and Late Miocene.These three times of tectonic movement had built the most important regional tectonic interfaces in the South China Sea.Crust movement of the South China Sea was the result and epitome of interaction of the Eurasia,Pacific and Indo)Australia plates,that is,they were introduced by polycyclic changes of directions,rates and strengths of lithospheric movement and asthenospheric flow covering across the Pacific and Indo)Australia plates.
- South China Sea,
- Cenozoic,
- tectonic movement

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References(42)

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