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Stratigraphic architecture of the Neoproterozoic glacial rocks in the “Xiang-Qian-Gui” region of the central Yangtze Block, South China
引用本文: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). Stratigraphic architecture of the Neoproterozoic glacial rocks in the “Xiang-Qian-Gui” region of the central Yangtze Block, South China[J]. 自然科学进展(英文版), 2003, 13(10). DOI: 10.1080/10020070312331344430
作者姓名: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)
作者单位: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
基金项目:SupportedbytheNationalNaturalScienceFoundationofChina (GrantNo .40 172 0 15 )andtheChineseAcademyofSciences (GrantNo .KZCX2 116)
摘    要:Recently ,theinterestinglowlatitudeandlowaltitudeSnowballEarthhypothesis[1,2 ] iswidelyreco gnized ,and greatlystimulatingthestudyoftheNeoproterozoicglaciations ,whichmaybecloselyre latedtothewell knownEarlyCambrianbio radiationevent.By 1980 ,theNeoproterozoicglaciationinSouthChinaisbelievedtobedividedintotwoglaciationsandoneinterglaciation[3~ 5] ,namely ,theearlyChang’anGlaciation ,lateNantuoGlaciationandFu luInterglaciation .However ,thereweredifferentwaysofcorrelation ,themostobvious…


Stratigraphic architecture of the Neoproterozoic glacial rocks in the "Xiang-Qian-Gui" region of the central Yangtze Block, South China
ZHANG Qirui,Chu Xuelei,Heinrich BAHLBURG,FENG Lianjun,Nicole DOBRZINSKI,ZHANG Tonggang. Stratigraphic architecture of the Neoproterozoic glacial rocks in the "Xiang-Qian-Gui" region of the central Yangtze Block, South China[J]. Progress in Natural Science, 2003, 13(10). DOI: 10.1080/10020070312331344430
Authors:ZHANG Qirui  Chu Xuelei  Heinrich BAHLBURG  FENG Lianjun  Nicole DOBRZINSKI  ZHANG Tonggang
Abstract: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.
Keywords:Neoproterozoic glacial rocks   central Yangtze Block   stratigraphic architecture   classification and correlation   stratigraphic break.
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