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Minghui Yang
China University of Petroleum
7Publications
4H-index
88Citations
Publications 7
Newest
#1Shaohua ZhangH-Index: 2
#2Chiyang LiuH-Index: 6
Last.Hexin HuangH-Index: 8
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#1Shaohua Zhang (Northwest University (United States))H-Index: 2
#2Chiyang Liu (Northwest University (United States))H-Index: 6
Last.Jianqiang Wang (Northwest University (United States))H-Index: 2
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2 CitationsSource
#1Chaoli Lan (China University of Petroleum)H-Index: 2
#2Minghui Yang (China University of Petroleum)H-Index: 4
Last.Yongzhong Zhang (PetroChina)H-Index: 1
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Abstract The Pennsylvanian Taiyuan Formation of the Shenmu Field in the northeastern Ordos Basin of China contains tight sandstone reservoirs that have recently been commercially produced. An evaluation of the reservoir quality of the Taiyuan sandstones will play a critical role in the development of the field. An investigation was conducted to explore possible effects of the sequence stratigraphy, depositional facies and diagenetic alterations on the reservoir quality of the Taiyuan sandstones ...
11 CitationsSource
#1Minghui Yang (China University of Petroleum)H-Index: 4
#2Liang Li (Sinopec)H-Index: 2
Last.Chao Ding (China University of Petroleum)H-Index: 1
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Abstract This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this su...
20 CitationsSource
#1Minghui Yang (China University of Petroleum)H-Index: 4
#2Zhijun Jin (Sinopec)H-Index: 17
Last.Peng Zeng (China University of Petroleum)H-Index: 1
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The Baicheng (拜城) piggy-back basin was part of the intracontinental foreland basin system of southern Tianshan (天山) Mountains. It was formed on a thrust-and-fold belt induced by Mio-Pliocene collision between southern Tianshan Mountains and Tarim craton that controlled the thick synorogenic basin fills. Sedimentological analysis and a restored cross-section based on seismic data and field studies revealed three tectono-depositional sequences of synorogenic basin fills. (1) The Lower Miocene sequ...
1 CitationsSource
#1Minghui Yang (China University of Petroleum)H-Index: 4
#2Zhijun Jin (Sinopec)H-Index: 17
Last.Ganglin Lei (CNPC: China National Petroleum Corporation)H-Index: 3
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: The eastern Qiulitagh fold and thrust belt (EQFTB) is part of the active Kuqa fold and thrust belts of the northern Tarim Basin. Seismic reflection profiles have been integrated with surface geologic and drill data to examine the deformation and structure style of the EQFTB, particularly the deformational history of the Dina 2 gas field. Seismic interpretations suggest that Dongqiu 8 is overall a duplex structure developed beneath a passive roof thrust, which generated from a tipline in the Mi...
15 CitationsSource
#1Zhijun Jin (Sinopec)H-Index: 17
#2Minghui Yang (China University of Petroleum)H-Index: 4
Last.Ganglin Lei (CNPC: China National Petroleum Corporation)H-Index: 3
view all 7 authors...
The timing of hydrocarbon charging relative to trap formation is a key factor for evaluating the exploration potential of the Qiulitagh fold and thrust belt (QFTB) on the north flank of the Tarim basin. Data obtained by this study indicate that structural traps were filled by hydrocarbons in two episodes. In this area, at least four major deformation events have been identified for the period of Late Cretaceous to Pliocene. The first event occurred in Late Cretaceous and led to the formation of ...
39 CitationsSource
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