Shuai Yang
Chengdu University of Technology
20 Papers
15 Citations
Shuai Yang is an academic researcher from Chengdu University of Technology. The author has contributed to research in topics: Geology & Permian. The author has an hindex of 5, co-authored 14 publications.
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Papers
Characteristics, formation and evolution of pre-salt dolomite reservoirs in the fifth member of the Ordovician Majiagou Formation, mid-east Ordos Basin, NW China
Siyi Fu,Chenggong Zhang,Hongde Chen,Anqing Chen,Junxing Zhao,Zhongtang Su,Shuai Yang,Guo Wang,Wentian Mi +8 more
TL;DR: The characteristics and formation of pre-salt dolomite reservoirs in the fifth member of Ordovician Majiagou Formation in the mid-east Ordos Basin are investigated through observation of cores and thin sections, and geochemical analysis.
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Source-to-sink of Late carboniferous Ordos Basin: Constraints on crustal accretion margins converting to orogenic belts bounding the North China Block
Anqing Chen,Anqing Chen,Hao Zou,Hao Zou,Hao Zou,James G. Ogg,James G. Ogg,Shuai Yang,Mingcai Hou,Xiuwei Jiang,Shenglin Xu,Xiaoxing Zhang +11 more
TL;DR: In this paper, an integrated analysis of stratigraphy, petrography, and U-Pb dates and Hf isotopes on detrital zircons was performed to investigate its provenance and relationships to the progressive collisions that formed the Xing’an-Mongolia Orogenic Belt to the north and the Qinling Orogenetic Belt to south.
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Ordovician deep dolomite reservoirs in the intracratonic Ordos Basin, China: Depositional model and Diagenetic evolution:
Anqing Chen,Anqing Chen,Shenglin Xu,Shuai Yang,Hongde Chen,Zhongtang Su,Yijiang Zhong,Yijiang Zhong,Sihan Hu +8 more
TL;DR: In this paper, the sedimentological and geochemical characteristics of the Ordos Basin were examined, and it was shown that non-karstification dominated reservoirs exist in the basin.
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Early Permian chemical weathering indices and paleoclimate transition linked to the end of the coal-forming episode, Ordos Basin, North China Craton
Shi Sun,Anqing Chen,Hongde Chen,Mingcai Hou,Shuai Yang,Shenglin Xu,Feng Wang,Zhifa Huang,James G. Ogg,James G. Ogg +9 more
TL;DR: In this article, a chemical weathering study on the Shanxi and Xiashihezi formations in the Ordos Basin of the North China Craton (NCC) was conducted to explore whether a change in paleoclimatic conditions may have been a factor in coal-forming episode termination.
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Rapid climatic fluctuations during the Guadalupian-Lopingian transition: Implications from weathering index recorded in acid-insoluble residua of carbonate rocks, South China
Shine Soon Sun,Y. Q. Chen,Ming Cai Hou,Shuai Yang,James G. Ogg,Hao Zou,Qian Li,Yifan Huang,Ruixuan Li,Hongde Chen +9 more
TL;DR: In this article , the Guadalupian-Lopingian boundary (GLB) transition was regarded as a gradual warming period with the termination of the Late Paleozoic Ice Age (LPIA), however, the glacial-nonglacial cycles from Eastern Australia imply that the period was also influenced by climatic fluctuations.
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