Citation: | ZHANG Yong, YAO Yongjian, LI Xuejie, SHANG Luning, YANG Chupeng, WANG Zhongbo, WANG Mingjian, GAO Hongfang, PENG Xuechao, HUANG Long, KONG Xianghuai, WANG Jun, MI Beibei, ZHONG Hexian, CHEN Hongjun, WU Hao, LUO Weidong, MEI Xi, HU Gang, ZHANG Jiangyong, XU Ziying, TIAN Zhixian, WANG Zhe, LI Xia, WANG Zhonglei. 2020. Tectonic evolution and resource-environmental effect of China Seas and adjacent areas under the multisphere geodynamic system of the East Asia ocean-continent convergent belt since Mesozoic[J]. Geology in China, 47(5): 1271-1309. doi: 10.12029/gc20200501 |
The Mesozoic-Cenozoic tectonic activity in eastern China was mainly controlled by the interaction of the Pacific plate and the Philippine plate with the Eurasian plate. In recent years, the concept of multisphere tectonics of earth system has provided a new perspective for understanding the interaction between various layers of the East Asian convergence system. Based on the 1:1 million marine regional geological survey, this paper comprehensively summarizes the geological structure of China's sea areas and their adjacent areas, initially forming the "multisphere interactions in East Asia ocean-continent convergence zone" with the core of "one margin, two-stage subduction, three-stage extension, and hierarchical control". In addition, a new first-order tectonic unit division scheme was first proposed in the region between the oceanic plate and the continental margin, referred to as "East Asia continental margin convergence zone". According to the differences of tectonic evolution, this tectonic unit could be roughly divided into the northern Japan-Ryukyu section and the southern Philippine section based on Taiwan Island. "East Asia continental margin convergence zone" has provided a powerful explanation for the geodynamic process of multiple geotectonic events in East Asia under the West Pacific subduction and Philippine Sea plate subduction system since the Meso-Cenozoic. It formed geomorphic features in China's sea areas which show zonal variation in East China's sea areas and cyclic variation in South China's sea areas. The geomorphic framework further caused the sedimentary differentiation model of "Great River-Great Delta-Terrigenous-Banded" and "Short source river-High angle slope-Multisource-Annular" in East and South China's sea areas, respectively.
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The geotectonic location of East Asia continental margin convergence zone (modified from Li Sanzhong et al., 2018)
Bouguer gravity anomaly map(a)and Moho depth map (b) of China's seas and adjacent areas
Topographic and structural characteristics of the northern—middle (a, b) and southern (c) parts of the Diaoyudao Uplift and Okinawa Trough (after Shang Luning et al., 2018a)
The geometric, kinematic and dynamic characteristics of the fault zone in the western margin of the South China Sea
The structural characteristics of the subduction zone in the east margin of South China Sea
The structural characteristics of Zhongnan-Liyue fault zone
The seismic reflection characteristics of Meiji reef fault zone
The structural outline of China seas and adjacent areas
Early-Middle Jurassic tectonic evolution of China seas and adjacent areas
Late Jurassic-Cretaceous tectonic evolution of China seas and adjacent areas
Late Cretaceous-Oligocene tectonic evolution of China seas and adjacent areas
Geomorphic types of China seas and adjacent areas
The surface sediments differentiation in China seas and adjacent areas
The comparison of source, reservoir and cap conditions in typical petroliferous basins
The distribution map of building sand of the buried ancient channel type in the Yellow Sea shelf area
The fluid circulation model of the typical subsea hydrothermal active zone in the Okinawa Trough(after Shang Luning et al., 2017)