Mesozoic collision—extrusion tectonics in eastern Asia

Mesozoic collision—extrusion tectonics in eastern Asia
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DOI:
10.1016/0040-1951(90)90005-s
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发表时间:
1990-09
期刊:
影响因子:
2.9
通讯作者:
G. Kimura;Masaki Takahashi;M. Kono
G. Kimura;Masaki Takahashi;M. Kono
中科院分区:
地球科学2区
文献类型:
--
作者:
G. Kimura;Masaki Takahashi;M. Kono

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早白垩纪亚洲大陆东部变形剧烈。变形被解释为与东部大陆边缘的俯冲构造有关。我们提出了一种由印度支那地块与欧亚大陆碰撞而产生的碰撞-挤压构造的替代构造框架。这一事件控制了东亚侏罗纪至白垩纪的构造史和大陆东缘俯冲带的演化。
The eastern part of the Asian continent was intensively deformed in early Cretaceous time. Deformation has been interpreted to be related to subduction tectonics along the eastern continental margin. We propose an alternative tectonic framework of collision—extrusion tectonics resulting from collision of the Indochina Block with the Eurasian continent. This event controlled the Jurassic to Cretaceous tectonic history in eastern Asia and the evolution of the subduction zone along the eastern margin of the continent.