From passive continental margin to active continental margin: basin recordings of Mesozoic tectonic regime transition of the East China Sea Shelf Basin
Hou Fanghui1,2, Zhang Xunhua1,2, Li Gang1,2, Li Sanzhong3, Wen Zhenhe1,2, Li Rihui1,2
1. Key Laboratory of Marine Hydrocarbon Resource and Geology, Ministry of Land and Resources, Qingdao, Shandong 266071, China;
2. Qingdao Institute of Marine Geology, Qingdao, Shandong 266071, China;
3. Ocean University of China, Qingdao, Shandong 266003, China
Abstract:Located at the East Asia continental margin, the East China Sea Shelf Basin is a Mesozoic-Cenozoic composite basin superposed on the South China Block. Research on Mesozoic tectonic regime transition and evolution process in the basin is of great significance for good understanding tectonic evolution in the South China. This paper presents our research on the distribution of Mesozoic strata and tectonic characteristics using new seismic data acquired in recent years. Based on our research work, it is a depression basin in the Jurassic period and a fault depression basin in the Cretaceous period. Through the structural evolution section recovery and combined with regional sea-land tectonic contrast, the Mesozoic evolution process is divided into three stage: passive continental margin depression stage in the late Triassic-middle Jurassic, Andean active continental margin arc uplift stage in the late Jurassic-early Cretaceous, and West Pacific active continental margin back-arc stretch basin stage in the late early Cretaceous-late Cretaceous.
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