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Stratigraphic architecture of the neoproterozoic glacial rocks in the “Xiang-Qian-Gui” region of the central Yangtze Block, South China

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Progress in Natural Science:Materials International 2003年第10期 63-67页

作者： ZHANG Qirui 1*, CHU Xuelei 1, Heinrich BAHLBURG 2, FENG Lianjun 1, Nicole DOBRZINSKI 2 and ZHANG Tonggang 1(1. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China 2. Geologisch Palaeontologisches Institut, Westfaelische Wilhelms Universitaet, Corrensstrasse 24, D 48149 Muenster, Germany) Institute of Geology and Geophysics Chinese Academy of Sciences Beijing 100029 China Geologisch-Palaeontologisches Institut Westfaelische Wilhelms-Universitaet Corrensstrasse 24 D-48149 Muenster Germany

The Yangtze Block in South China is one of the important regions where neoproterozoic glacial rocks are well developed and studied. However, the classification and correlation of the neoproterozoic glacial sequences in the central Yangtze Block still remain controversial among Chinese geologists. The original Sinian sections around the Yangtze Gorges Region became an official standard for classification and correlation since the 1950s. Subsequent regional geologic studies, however, resulted in different classification and correlation, because of its incompleteness. We select one of the complete sections in the bordering areas of Xiang (Hunan), Qian (Guizhou) and Gui (Guangxi), as a standard of classification and correlation. The temporal and spatial distribution, i.e. the stratigraphic architecture, of the glacial rocks in the central Yangtze Block is suggested. Our results indicate that the glacial sequence on the Yangtze Block was deposited during the Nantuo Ice age, the Datangpo Interglacial age and Jiangkou Ice age, in descending order.

关键词： neoproterozoic glacial rocks central Yangtze Block stratigraphic architecture classification and correlation stratigraphic break.

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Stratigraphic architecture of the neoproterozoic glacial rocks in the“Xiang-Qian-Gui”region of the central Yangtze Block,South China

Stratigraphic architecture of the Neoproterozoic glacial roc...

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中国科学院地质与地球物理研究所2003学术年会

作者： Heinrich BAHLBURG Nicole DOBRZINSKI Geologisch-Palaeontologisches Instirut Westfaelische Wilhelms-UniversitaetCorrensstrasse 24D-48149 MuensterGermany

The Yangtze Block in South China is one of the important regions where neoproterozoic glacial rocks are well developed and ***,the classification and correlation of the neoproterozoic glacial sequences in the central Yangtze Block still remain controversial among Chinese *** original Sinian sections around the Yangtze Gorges Region became an official standard for classification and correlation since the *** regional geologic studies,however,resulted in different classification and correlation, because of its *** select one of the complete sections in the bordering areas of Xiang(Hunan),Qian(Guizhou)and Gui(Guangxi),as a standard of classification and *** temporal and spatial distribution,*** stratigraphic architecture,of the glacial rocks in the central Yangtze Block is *** results indicate that the glacial sequence on the Yangtze Block was deposited during the Nantuo lce-age,the Datangpo Interglacial-age and Jiangkou lce-age,in descending order.

关键词： neoproterozoic glacial rocks central Yangtze Block stratigraphic architecture classification and correlation stratigraphic break

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