东海陆架盆地中新生代构造背景及演化

doi:10.11743/ogg20050210

石油与天然气地质 ›› 2005, Vol. 26 ›› Issue (2): 197-201.doi: 10.11743/ogg20050210

东海陆架盆地中新生代构造背景及演化

郑求根^1,2, 周祖翼², 蔡立国¹, 陆永德¹, 曹清古¹

1. 中国石化石油勘探开发研究院无锡实验地质研究所, 江苏无锡, 214151;
2. 同济大学海洋地质与地球科学学院, 上海, 200092

收稿日期:2005-04-01 出版日期:2005-04-25 发布日期:2012-01-16
基金项目:
中国石化科技项目"中国东部海域盆地构造演化与油气勘探方向"(P03072)

Meso-Cenozoic tectonic setting and evolution of East China Sea shelf basin

Zheng Qiugen^1,2, Zhou Zuyi², Cai Liguo¹, Lu Yongde¹, Cao Qinggu¹

1. Wuxi Branch of Exploration and Production Research Institute, SINOPEC, Wuxi, Jiangsu;
2. College of Marine Geology & Earth Science, Tongji University, Shanghai

Received:2005-04-01 Online:2005-04-25 Published:2012-01-16

摘要/Abstract

摘要：

从东海中生界的分布和闽浙东部岩浆构造事件来看,侏罗纪—早白垩世库拉-太平洋板块已对中国大陆有较强的俯冲作用,东海及其以南地区应为弧前盆地性质。晚白垩世晚期—始新世,火山岛弧向东移动,东海陆架盆地变为弧后盆地。古新世的断陷中心在东海陆架盆地西部的长江凹陷、瓯江凹陷。始新世时,断陷中心向东迁移,以陆架盆地东部的西湖凹陷为主。到了渐新世,由于太平洋板块俯冲方向的改变以及菲律宾海板块的作用,东海陆架盆地发生坳陷,坳陷中心以东部为主。中新世晚期,冲绳海槽和疏球岛弧形成。晚中新世(约6Ma),吕宋岛弧在台湾地区与中国大陆发生碰撞,台湾岛上升露出水面,形成了台西盆地现今的面貌。

关键词: 东海陆架盆地, 中新生代, 太平洋板块, 菲律宾海板块, 构造演化

Abstract:

Based on distribution of Mesozoic in East China Sea and magmatic-tectonic events in the eastern Fujian and Zhejiang provinces, Kula-Pacific plate would have relatively strong subduction toward China's mainland during Jurassic-Early Cretaceous, thus East China Sea and the area to the south should be of fore-arc basin. During late Late Cretaceous-Eocene, volcanic island arc moved eastward and the East China Sea shelf basin was turned into a back-arc basin. The centers of fault subsidence were located in Changjiang and Oujiang sags in the western part of the shelf basin during Palaeocene, and they moved eastward during Eocene and consisted mainly of the Xihu sag in the eastern part of the shelf basin. East China Sea shelf basin was downwarped in Oligocene, due to the change of subduction direction of Pacific plate and the effect of Philippine Sea plate, and the center of depression was mainly located in the eastern part. Okinawa ocean trough and Ryukyu island arc were formed in late Miocene. During late Miocene (approx. 6 Ma), Luzon island arc collided with China's mainland in Taiwan area, resulting in the emergence of Taiwan Island, and the formation of the present features of Taixi(or West Taiwan) basin.

Key words: East China Sea shelf basin, Meso-Cenozoic, Pacific plate, Philippine Sea plate, tectonic evolution

中图分类号:

TE111.2

郑求根,周祖翼,蔡立国,等. 东海陆架盆地中新生代构造背景及演化[J]. 石油与天然气地质, 2005, 26(2): 197-201. doi: 10.11743/ogg20050210 Zheng Qiugen,Zhou Zuyi,Cai Liguo,et al. Meso-Cenozoic tectonic setting and evolution of East China Sea shelf basin[J]. Oil & Gas Geology, 2005, 26(2): 197-201. doi: 10.11743/ogg20050210

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东海陆架盆地中新生代构造背景及演化

Meso-Cenozoic tectonic setting and evolution of East China Sea shelf basin

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