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Devonian Sequence Stratigraphy and Sea Level Change Cycles in South China 被引量:3
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作者 Du Yuansheng Gong Yiming (Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074) Wu Yi (Guangxi Institute of Geology, Nanning 530023) Liu Benpei Feng Qinglai (Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074) 《Journal of Earth Science》 SCIE CAS CSCD 1996年第1期72-79,共8页
The Devonian is well developed in South China and has drawn a great attention from the geologists both at domestic and abroad. On the basis of study on the sequence stratigraphy in more than 10 sections in Guizhou, Gu... The Devonian is well developed in South China and has drawn a great attention from the geologists both at domestic and abroad. On the basis of study on the sequence stratigraphy in more than 10 sections in Guizhou, Guangxi, Longmenshan and Southern Qinling within South China we have identified 21 sequences and T-R cycles that correspond to third-order sea level changes. These sea level change cycles were controlled by autorhythm(Pragian,Eifelian), allorhythm(Lochkovian,Emsian,Givetian) and coupling rhythm mechanisms (frasian, Famennian and F-F boundary). 展开更多
关键词 south China Devonian sequence sea level change cycle.
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