引用本文:吴基文, 陈资平.安徽南部晚二叠世龙潭期岩相古地理研究[J].沉积与特提斯地质,1997,(5):40-49.[点击复制]
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安徽南部晚二叠世龙潭期岩相古地理研究
吴基文,陈资平
0
(淮南矿业学院)
摘要:
本文系统地讨论了皖南地区晚二叠世早期沉积层发育特征,确定了龙潭期地层的顶、底界线。以单因素图件为基础,结合其它成因标志,编制了龙潭早期(三个亚期)和龙潭晚期岩相古地理图。由此可以看出龙潭期的岩相古地理特征及其演化历史。
关键词:  龙潭期  岩相古地理  安徽南部  层序地层
DOI:
附件
基金项目:
SEDIMENTARY FACIES AND PALAEOGEOGRAPHY IN SOUTHERN ANHUI DURING THE LONGTANIAN (LATE PERMIAN)
Wu Jiwen, Chen Ziping
(Huainan Mining College)
Abstract:
The early Longtanian(Late Permian)sedimentary strata are obviously governed by bedrock relief in southern Anhui.The sedimentary strata were laid down initially in the to-pographic lows,and then progressively overlapped upon the topographic highs.This dis-trict was an epeiric sea basin during the late Longtanian,and at the latest of the stage,ex-hibited a shallowing trend of sea water.Therefore there are large discrepancies in lithology and lithofacies of the sedimentary strata and ecological environments of the organisms in the study area.The present paper discusses the characteristics of the early Late Permian sedimentary strata and delineates the top and bottom boundaries of the Longtanian strata. Moreover the sedimentary facies and palaeogeographic maps during three substages of the early Longtanian have been compiled in the light of monofactor charts and diagrams in combination with relevant genetic indicators.The results of research in this paper may im-prove our knowledge of understanding in the evolution of the early Late Permian sedimen-tary facies and palaeogeography,and the initiation and development of coal-forming pro-cesses in southern Anhui.
Key words:  Longtanian  sedimentary facies and palaeogeography  southern Anhui  sequence stratigraphy

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