North-south segmentation and horizontal movementof the East China Sea micro-plate

Lin Changsong; Gao Jinyao

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Lin Changsong, Gao Jinyao. North-south segmentation and horizontal movementof the East China Sea micro-plate[J]. Haiyang Xuebao, 1999, 21(1): 80-89.

Citation:

Lin Changsong, Gao Jinyao. North-south segmentation and horizontal movementof the East China Sea micro-plate[J]. Haiyang Xuebao, 1999, 21(1): 80-89.

Lin Changsong, Gao Jinyao. North-south segmentation and horizontal movementof the East China Sea micro-plate[J]. Haiyang Xuebao, 1999, 21(1): 80-89.

Citation:

Lin Changsong, Gao Jinyao. North-south segmentation and horizontal movementof the East China Sea micro-plate[J]. Haiyang Xuebao, 1999, 21(1): 80-89.

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North-south segmentation and horizontal movementof the East China Sea micro-plate

Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012

Received Date: 1997-09-18
Rev Recd Date: 1997-12-26

Abstract

Abstract

Before Upper Cretaceous, the Paleo-Minzhe-the Paleo-Korea trench-arc system and the Ryukyu trench-arc system constitute the old double-subduction zone. The tectonic movement of the East Clung Sea micro-plate was subjected to the old double-subduction zone. The north-south segmentation of the basement of the East China Sea and the Ryūkyū trench-arc system,cutted by the NW-trending faults, is of different features in the each part. Subduction of substance and stress was changed along the different zone of the western old double trench-arc systems, such a double subduction zone accompanied differential adjustment of the crust horizontal stress with the NW-trending faults.
- China Sea micro-plate,
- north south segmentation,
- double-subduction zone

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References(30)

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