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湘鄂赣二叠纪岩相古地理研究
引用本文:牟传龙,丘东洲,王立全,万方.湘鄂赣二叠纪岩相古地理研究[J].沉积与特提斯地质,1997,17(6):1-21.
作者姓名:牟传龙  丘东洲  王立全  万方
作者单位:地矿部成都地质矿产研究所
基金项目:地质矿产部沉积盆地与流体动力学开放研究实验室成果:97013
摘    要:湘鄂赣二叠纪沉积盆地是在华南陆块基础上发育而成,具有扬子克拉通北缘被动大陆边缘盆地,扬子克拉通盆地,湘赣板内拉张盆地和华夏克拉通边缘盆地等四类。根据古暴露等标志,建立了各类盆地的沉积层序,并进行了区域对比。

关 键 词:岩相  古地理  沉积体系域模式  沉积盆地  二叠纪

PERMIAN SEDIMENTARY FACIES AND PALAEOGEOGRAPHY IN THE HUNAN-HUBEI-JIANGXI REGION
Mou Chuanlong,Qiu Dongzhou,Wang Liquan,Wan Fang.PERMIAN SEDIMENTARY FACIES AND PALAEOGEOGRAPHY IN THE HUNAN-HUBEI-JIANGXI REGION[J].Sedimentary Geology and Tethyan Geology,1997,17(6):1-21.
Authors:Mou Chuanlong  Qiu Dongzhou  Wang Liquan  Wan Fang
Institution:Chengdu Institute of Geology and Mineral Resources, CAGS
Abstract:The Permian sedimentary basins in the Hunan-Hubei-Jiangxi region developed on the South China continental block are classified into the passive marginal basin on the northern margin of the Yangtze craton,Yangtze craton basin,Hunan-Hubei-Jiangxi intraplate exten-sional basin and Hercynian pericratonic basin.The sedimentary sequences in individual basins have been established and correlated regionally in the light of fossil exposures. Moreover the sedimentary facies and palaogeographic maps of the Hunan-Hubei-Jiangxi re-gion have been worked out,and models for the depositional systems tracts proposed in the present paper.
Keywords:sedimentary facies and palaeogeography  model for depositional systems tract  Permian  Hunan-Hubei-Jiangxi region
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