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《Geological Journal of China Universitiesf》 2000-04
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Study on Sinian Geologic Events in Xuzhou-Suzhou Area and Discussion on Their Origin

PAN Guo qiang, LIU Jia run, KONG Qing you, WU Qun qi, ZHANG Qing long, ZENG Jia hu, LIU Dao zhong (Department of Earth Sciences, Nanjing University, Nanjing 210093, China)  
The Sinian strata in Xuzhou Suzhou area are deposits of the epicontinental sea. They are mainly referred to the carbonate platform facies. In the supratidal to subtidal low energy sedimental environments, sudden, violent high energy sedimentation occasionally occur, which are often associated with some abnormal sedimentary structures. These structures along with step like small faults may indicate the ancient seismic traces. In the studied area, the Sinian seismic traces mainly include densely spaced veins of micritic calcites, strongly scouring and erosion structures of "bag gutter" like, plastic rudites, earthquake breccias, inter formation folds and step like small faults. Five distinguished stratomeres with closely spaced seismic traces represen ting five earthquakes phases have been recognized, which might include dozens, even hundreds of strong earthquakes. At least two phases of hypabyssal to subsurface basic magmatic intrusions can be distinguished, occurring respectively in the early and late Sinian period. The seismic events, magmatic intrusions and sea level changes are related in origin. Frequent, strong earthquake activities caused the sea level rise. The magmatic intrusions occurred in the interval between tow seismic phases and in the sea level fall times. The research results showed that the Sinian geologic events in the studied area might be controlled by extensional structures. The ages of these events are 738.6-604Ma, corresponding to the breakup times (780-600Ma) of global supercontinent Rodinia. Therefore it is deduced that the origin of the Sinian geologic events in Xuzhou Suzhou area might relate to the breakup processes of Rodinia. The area from "Plaeo Tanlu zone" to the north of boundary fault zone in the northern side of North Qinling Mountains might be the breakup zone within the North China Plate margin.
【Fund】: 国土资源部区调项目(1∶5万房村幅、双沟幅区域地质调查 )资助
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