Late Carboniferous-Early Permian Sequence Stratigraphy and Depositional Evolution in the Northeast Ordos Basin, North China

被引:14
|
作者
Yang Minghui [1 ,2 ]
Liu Chiyang [3 ]
Lan Chaoli [4 ]
Liu Le [5 ]
Li Xin [2 ]
Zhang Kunshan [2 ]
机构
[1] China Univ Petr, State Key Lab Petr Resource & Prospecting, Beijing 102249, Peoples R China
[2] China Univ Petr, Coll Geosci, Beijing 102249, Peoples R China
[3] NW Univ Xian, State Key Lab Continental Dynam, Xian 710069, Shaanxi, Peoples R China
[4] China Univ Petr, Coll Petr Engn, Beijing 102249, Peoples R China
[5] PetroChina, Res Inst BGP, Zhuozhou 072751, Hebei, Peoples R China
关键词
sequence stratigraphy; sedimentary facies; depositional evolution; Late Paleozoic; Ordos Basin; ACCUMULATION;
D O I
10.1111/j.1755-6724.2010.00292.xL
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
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.
引用
收藏
页码:1220 / 1228
页数:9
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