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《Geology of Anhui》 2011-01
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<TITLE>PERMIAN DEPOSITS AND THEIR EVOLUTIONAL FEATURES IN XINGTAN,ZIGUI,HUBEI

WAN Qiu1,LI Shuang-ying1,DING Ning2,KONG Wei-lun1(1 School of Resources and Environmental Engineering,Hefei University of Technology,Hefei,Anhui 230009,China;2 Geological Survey of Anhui Province,Hefei,Anhui 230001,China)  
The stratigraphy is well outcropped with distinctive features in the Xingtan area,Zigui,Hubei province.On the basis of previous work made in the area,this paper divided Permian lithofacies and deposit and preliminarily studied the sedimentary evolution by using measured cross-sections,sedimentary facies analysis combined with microfacies and paleotology.Lithofacies analysis indicates that mid-upper Permian series in the study area comprises mainly bioclast limestone,micrite,calcrenite,calcirudite,silicolite,etc.Sedimentary facies analysis suggests that the mid-upper Permian consists primarily of carbonate slope and platform deposit,secondarily of shoreland and basinal deposit.The mid-Permian consists of two developed transgression-regression cycles respectively of the Qixia and Maokou times,and the late Permian is characterized by open platform deposit of the Wujiaping time,with 2 and a half cycles as a whole.
【Fund】: 国家自然科学基金(40572076);; 安徽省自然科学基金资助项目(9075507);; 中国石油化学工业总公司海相前瞻性课题《古特提斯构造演化与中上扬子油气中组合研究》
【CateGory Index】: P512.2
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