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Late Carboniferous–Early Permian Sequence Stratigraphy and Depositional Evolution in the Northeast Ordos Basin, North China
作者姓名:YANG Minghui  LIU Chiyang  LAN Chaoli  LIU Le  LI Xin and ZHANG Kunshan
作者单位:1 State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China; 2 College of Geosciences, China University of Petroleum, Beijing 102249, China; 3 State Key Laboratory of Continental Dynamics, Northwest University, Xi’an, Shaanxi 710069, China; 4 College of Petroleum Engineering, China University of Petroleum, Beijing 102249, China; 5 Research Institute of BGP, PetroChina, Zhuozhou, Hebei 072751, China
基金项目:This study is financially supported by the National Major Fundamental Research and Development Project of China (Grant No. 2003CB214600) and the State Key Program of National Natural Science of China (Grant No. 90814005).
摘    要:Sequence stratigraphical analysis was applied to the Upper Carboniferous–Lower Permian sedimentary succession of the northeastern Ordos Basin, north China based on data acquired from ten entire logging curves and eight outcrops. The facies framework of the lithostratigraphical unit, the Taiyuan Formation comprises seven facies in two facies associations, varying from fluvio-delta to shelf-barrier islands. The facies are presented within a chronostratigraphical framework, linked by systems tract, which in turn are limited by flooding surfaces and sequence boundaries. Six third-order depositional sequences are recognised, bounded by six type 2 unconformities. An upwards-shallowing epicontinental sea sedimentary model is created, which consists of a sandstone, coal seam and carbonate succession.

关 键 词:sequence  stratigraphy    sedimentary  facies    depositional  evolution    Late  Paleozoic    Ordos  Basin
收稿时间:4/1/2010 12:00:00 AM
修稿时间:9/1/2010 12:00:00 AM

Late Carboniferous‐Early Permian Sequence Stratigraphy and Depositional Evolution in the Northeast Ordos Basin,North China
Authors:YANG Minghui  LIU Chiyang  LAN Chaoli  LIU Le  LI Xin  ZHANG Kunshan
Institution:1. State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China;2. College of Geosciences, China University of Petroleum, Beijing 102249, China;3. State Key Laboratory of Continental Dynamics, Northwest University, Xi'an, Shaanxi 710069, China;4. College of Petroleum Engineering, China University of Petroleum, Beijing 102249, China;5. Research Institute of BGP, PetroChina, Zhuozhou, Hebei 072751, China
Abstract:Sequence stratigraphical analysis was applied to the Upper Carboniferous‐Lower Permian sedimentary succession of the northeastern Ordos Basin, north China based on data acquired from ten entire logging curves and eight outcrops. The facies framework of the lithostratigraphical unit, the Taiyuan Formation comprises seven facies in two facies associations, varying from fluvio‐delta to shelf‐barrier islands. The facies are presented within a chronostratigraphical framework, linked by systems tract, which in turn are limited by flooding surfaces and sequence boundaries. Six third‐order depositional sequences are recognised, bounded by six type 2 unconformities. An upwards‐shallowing epicontinental sea sedimentary model is created, which consists of a sandstone, coal seam and carbonate succession.
Keywords:sequence stratigraphy  sedimentary facies  depositional evolution  Late Paleozoic  Ordos Basin
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