Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Yushun CAO"'
Publikováno v:
Shiyou shiyan dizhi, Vol 45, Iss 3, Pp 576-586 (2023)
Pore structure, as the focus of shale reservoir research, has important influence on the occurrence of shale oil. In this paper, 10 shale core samples from the 7th member of Triassic Yanchang Formation (Chang 7 member) in Huachi area, Ordos Basin wer
Externí odkaz:
https://doaj.org/article/a7cbd40f51994eb4a886e12f7cdcddb9
Autor:
Qiang LI, Guangdi LIU, Zezhang SONG, Mingliang SUN, Lianqiang ZHU, Xingwang TIAN, Kui MA, Dailin YANG, Yunlong WANG, Yushun CAO, Fuliang YOU
Publikováno v:
Shiyou shiyan dizhi, Vol 44, Iss 6, Pp 997-1007 (2022)
The Sinian-Cambrian tight carbonate strata locating on the northern slope (NS) of the paleo-uplift of central Sichuan Basin is the frontier for ultra-deep natural gas exploration. The tectonic evolution of the NS determined the accumulation process a
Externí odkaz:
https://doaj.org/article/989b6dbb3cfa441280a79e78b6cb8ea7
Autor:
Jianbang Wu, Shenglai Yang, Bowen Gan, Yushun Cao, Wei Zhou, Gen Kou, Ziqiang Wang, Qiang Li, Wengang Dong, Binbin Zhao
Publikováno v:
ACS Omega, Vol 6, Iss 36, Pp 23243-23261 (2021)
Externí odkaz:
https://doaj.org/article/85d83038c1be43c58cfbbd18ae1fc68f
Publikováno v:
SSRN Electronic Journal.
Autor:
Yishu Li, Guangdi Liu, Zezhang Song, Benjian Zhang, Mingliang Sun, Xingwang Tian, Dailin Yang, Yunlong Wang, Lianqiang Zhu, Yushun Cao
Publikováno v:
Journal of Asian Earth Sciences. 239:105417
Publikováno v:
Marine and Petroleum Geology. 109:279-290
Nitrogen isotope (δ15N) analysis has been used to evaluate depositional redox conditions in well-preserved sedimentary systems; however, fewer N-isotope studies have been performed to reconstruct the redox conditions in lacustrine shales. In this pa
Publikováno v:
Journal of Petroleum Science and Engineering. 195:107747
Hydrocarbon generating potential in source rocks is influenced by various controlling factors. Bottom water redox condition during source rock deposition is an important one among these factors and can directly control the organic matter enrichments