scholarly journals Reservoir characteristics of the first member of Middle Permian Maokou Formation in Sichuan Basin and its periphery and inspirations to petroleum exploration, SW China

2021 ◽  
Vol 48 (6) ◽  
pp. 1329-1340
Author(s):  
Chengpeng SU ◽  
Rong LI ◽  
Guoshan SHI ◽  
Huofu JIA ◽  
Xiaobo SONG
Keyword(s):  
Sichuan Basin ◽  
Petroleum Exploration ◽  
Middle Permian ◽  
Sw China ◽  
Reservoir Characteristics

scholarly journals The reservoir characteristics research of Devonian Jinbaoshi Formation, Northwest Sichuan Basin, SW China

Petroleum ◽  
2021 ◽  
Author(s):  
Shixuan Zhang ◽  
Xiucheng Tan ◽  
Hao Tang ◽  
Cheng Huang ◽  
Zhimin Jin ◽  
...  
Keyword(s):  
Sichuan Basin ◽  
Sw China ◽  
Reservoir Characteristics

Rare earth elements (REEs) geochemistry of Sinian-Cambrian reservoir solid bitumens in Sichuan Basin, SW China: potential application to petroleum exploration

2015 ◽  
Vol 52 (2) ◽  
pp. 298-316 ◽  
Author(s):  
Ping Gao ◽  
Guangdi Liu ◽  
Zecheng Wang ◽  
Chengzao Jia ◽  
Tongshan Wang ◽  
...  
Keyword(s):  
Rare Earth ◽  
Rare Earth Elements ◽  
Potential Application ◽  
Sichuan Basin ◽  
Petroleum Exploration ◽  
Sw China

Paleo-Heat Flow Anomaly at the End of Middle Permian in NE Sichuan Basin, SW China: Did an Ocean Trough Exist?

2013 ◽  
Vol 734-737 ◽  
pp. 139-146
Author(s):  
Chuan Qing Zhu ◽  
Song Rao ◽  
Sheng Biao Hu
Keyword(s):  
Heat Flow ◽  
Sichuan Basin ◽  
Vitrinite Reflectance ◽  
Middle Permian ◽  
Early Triassic ◽  
Late Permian ◽  
Sw China ◽  
Northeastern Sichuan ◽  
Igneous Activity ◽  
Northeastern Sichuan Basin

It is an issue whether the Kaijiang-Liangping area (in the northeastern Sichuan Basin, SW China) was a controversial ocean trough during Changxing age in the late Permian-early Triassic. Some vitrinite reflectance (Ro) profiles from wells in the northeastern Sichuan Basin show obvious breaks, and the breaks are coincident with the boundary between the middle Permian and late Permian. Based on the Ro data, the heat flow history in the northeastern Sichuan Basin was reconstructed. The result shows that the heat flow reached its peak value at the end of middle Permian (~260Ma). The spatiotemporal feature of the heat flow evolution is not in agreement with the fact that there was a Kaijiang-Liangping Trough existing in the late-Permian to early Triassic. The palaeo-heat flow anomaly was, in fact, a response to the igneous activity in late middle Permian.

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