Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Zhaotong Sun"'
Autor:
Yuan Zhang, Yan Ding, Jun Wang, Ruiqing Hou, Mingran Zheng, Delin Ma, Junfei Huang, Wenxiang Li, Qichao Zhao, Zhaotong Sun, Wancheng Li, Jie Wang, Shijie Zhu, Liguo Wang, Xiaochao Wu, Shaokang Guan
Publikováno v:
Journal of Materials Research and Technology, Vol 30, Iss , Pp 6498-6507 (2024)
Magnesium (Mg) is abundant in humans. Studies have shown that Mg2+ significantly affects physiological processes such as osteogenesis, osteoblast adhesion and motility, immunomodulation, and angiogenesis. Mg-based alloy porous scaffolds have attracte
Externí odkaz:
https://doaj.org/article/864637ac8dbd47b1b04fde0a407da656
Publikováno v:
Journal of Natural Gas Geoscience, Vol 7, Iss 1, Pp 27-37 (2022)
Tight oil is a great potential resource for unconventional oil exploration and development. Determining the content of adsorbed tight oil in sandstone reservoirs and the factors controlling its content is crucial for the evaluation and development of
Externí odkaz:
https://doaj.org/article/86333bd320c74bb691c5d4873e29fd0f
Publikováno v:
Journal of Natural Gas Geoscience, Vol 5, Iss 6, Pp 327-340 (2020)
In order to investigate pore structure characteristics of Wufeng and Longmaxi Formations shales in the Sichuan Basin, the organic geochemical parameter and petrologic experiments, N2 and CO2 adsorptions, field emission scanning electron microscopy an
Externí odkaz:
https://doaj.org/article/a9a98edf82494772a12c9f0c19925236
Autor:
Chengfu Lyu, Ying Zhang, Liyong Fan, Taotao Li, Qianshan Zhou, Chao Li, Zhaotong Sun, Xue Gao
Publikováno v:
Lithosphere, Vol 2021, Iss Special 1 (2022)
AbstractCarbonate cements are an important type of cement in Permian tight gas reservoirs in the Ordos Basin. Moreover, the distribution of carbonate cements in sandstone provides an important basis for studying the fluid mechanism and genesis of cem
Externí odkaz:
https://doaj.org/article/c5348aeba3dd47f6bf74e958df19a4e7
Publikováno v:
Geofluids, Vol 2022 (2022)
The Upper Ordovician Wufeng Formation and Lower Silurian Longmaxi Formation black shales are the critical targets for shale gas exploration in the Sichuan Basin of South China. The enrichment of organic matter (OM) in shale is the basis for the gener
Externí odkaz:
https://doaj.org/article/ead1d8a973944b0e9ce972a6a1da4ddd
Autor:
Chengfu Lyu, Xinmao Zhou, Xuesong Lu, Ying Zhang, Chao Li, Qianshan Zhou, Zhaotong Sun, Guojun Chen
Publikováno v:
Geofluids, Vol 2021 (2021)
Gas adsorption experiments are becoming one of the most common methods to quantify and analyze the pore structures of shale samples in the petroleum industry. In this regard, particle size of the specimen plays an important role in the results that c
Externí odkaz:
https://doaj.org/article/d18ee42dda6d4347ae249288d41cace2
Autor:
Chengfu Lyu, Xixin Wang, Xuesong Lu, Qianshan Zhou, Ying Zhang, Zhaotong Sun, Liming Xiao, Xin Liu
Publikováno v:
Geofluids, Vol 2020 (2020)
The Kuqa Basin is a typical foreland basin in northwest China, characterized by compressive foreland fold-and-thrust belts and a regionally distributed huge salt layer. A large number of overthrust faults, fault-related folds, and salt-related struct
Externí odkaz:
https://doaj.org/article/f5b2d760f9d248828160d883e534a6e3
Publikováno v:
Journal of Green Economy and Low-Carbon Development. 2:27-35
Autor:
Zhaotong Sun, Chengfu Lyu, Qianshan Zhou, Liming Xiao, Xixin Wang, Xin Liu, Xuesong Lu, Ying Zhang
Publikováno v:
Geofluids, Vol 2020 (2020)
The Kuqa Basin is a typical foreland basin in northwest China, characterized by compressive foreland fold-and-thrust belts and a regionally distributed huge salt layer. A large number of overthrust faults, fault-related folds, and salt-related struct
Autor:
Chengfu Lyu, Gongcheng Zhang, Ying Zhang, Zhaotong Sun, Ming Ma, Qianshan Zhou, Chao Li, Guojun Chen
Publikováno v:
Marine and Petroleum Geology. 126:104891
The provenance of Upper Oligocene to Upper Miocene sandstones in the western Qiongdongnan Basin was studied by zircon U–Pb ages. More than 200 zircon grains were separated from the sandstone of the Upper Oligocene Lingshui, Lower Miocene Sanya, and