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《Journal of Stratigraphy》 2006-01
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STUDY OF THE EARLY-MIDDLE JURASSIC TECTONO-STRATIGRAPHY IN THE JIANGXI-FUJIAN-GUANGDONG REGION, SE CHINA

WANG Bin, SHU Liang-shu, and YANG Zhen-yu( Department of Earth Sciences, Nanjing University, Nanjing, 210093 )  
To understand the geotectonic transition from paleo-Asian-Tethys regime to paleo-Pacific regime in SE China, this paper analyzed geological features of the Early Jurassic—Middle Jurassic sedimentary basins in the Jiangxi-Fujian-Guangdong region including distribution of basin, sedimentary features, petrological assemblages, and paleogeographic evolution, and so on. Study results suggest that 1) the paleogeographic framework of higher landform to the southeast side and depression to the northwestern side had been preliminarily developed during the Early Jurassic, which was revealed by sedimentary features from terrestrial coarser clastic rocks to fine clastic rocks from southeast to northwest; 2) during the Middle Jurassic, except the northern Guangdong-southern Jiangxi region, a further uplifting process that enhanced the Early Jurassic paleogeographic framework took place in the most part of SE China, causing an expansion of mountain relief toward inland. In some districts, the EW-striking strata and tectonic bo- dies were locally changed to NE-striking ones. The geodynamic setting was likely related to the subduction of paleo-Pacific plate along the Japanese continental margin; the western Fujian-southern Jiangxi rifting basin group of bimodal volcanic-intrusive rocks and the granitic magmatism dated at 170—180Ma in the Nanling region implied that paleo-Pacific magmatic activity had influenced these areas; 3) most areas of SE China belonged to paleo-Asian-Tethys tectonic regime in the Early-Middle Jurassic. From the Middle Jurassic, study area had gradually changed the paleo-Asian-Tethys tectonic regime to the paleo-Pacific tectonic regime; strong volcanic eruption and granitic intrusion dated at 130—110Ma and preponderant attitude of NE-striking strata and tectonic outline in the Southeast China demonstrated that during the Early Cretaceous, geotectonic transition from paleo-Asian-Tethys regime to paleo-Pacific regime had been performed. So the Middle Jurassic seems to be an important geological period of geotectonic transition from paleo-Asian-Tethys regime to paleo-Pacific regime. The eastern part of Nanling Mountains is likely the best candidate for starting geotectonic transition.
【Fund】: 国家自然科学基金项目(No.40172067、40132010、40572118);; 教育部研究项目;; 南京大学研究生教育创新研究项目;; 中国大陆超深钻工程和南京大学成矿作用国家重点实验室联合资助
【CateGory Index】: P548.2
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