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《Geology in China》 2013-06
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Characteristics of Ordovician sedimentary evolution in Hunan Province

GE Xiang-ying;MOU Chuan-long;ZHOU Ken-ken;LIANG Wei;Chengdu Center of Geological Survey China Geological Survey;Key Laboratory of Sedimentary Basin and Oil and Gas Resources Ministry of Land and Resources;  
Based on field survey, laboratory analysis of sedimentary strata and summarization of previous research results in Hunan Province, the authors divided the Ordovician tectonic and sedimentary evolution into four stages, i.e., rimmed carbonate platform-shelf-deep water basin in the Early Ordovician, carbonate ramp-shelfdeep basin in the Middle Ordovician, carbonate ramp-shelf-deep water basin-shelf margin at the early age of Late Ordovician, and confined shallow marine-deep water basin-shelf margin in the late period of the Late Ordovician. The northwestern Hunan in Yangtze craton experienced the evolution from the rimmed carbonate platform to carbonate ramp, and finally became a confined shallow sea, with the black shale gradually replacing carbonates in lithology. The central and southern Hunan located at the edge of the craton and the Cathaysia Block was always in a clastic shallow marine environment, and the center of the basin migrated constantly from southeast to northwest.
【Fund】: 国家重大科技专项(2011ZX05043-005);; 中国地质调查局项目(1212011120112);; 中石化股份有限公司勘探南方分公司页岩气资源评价项目联合资助
【CateGory Index】: P512.2
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