Zobrazeno 1 - 10
of 33
pro vyhledávání: '"Jiguang TANG"'
Autor:
Lingyu GAO, Kongquan CHEN, Jianlin LU, Jiguang TANG, Xiusong TUO, Douzhong ZHANG, Chunming YAN, Yizhen PANG
Publikováno v:
Shiyou shiyan dizhi, Vol 46, Iss 3, Pp 565-575 (2024)
This study explored the dynamic control and differences of tectonic action on the formation of conventional and unconventional gas reservoirs in Pingqiao area, southeastern Sichuan Basin. Based on seismic, geolo-gical, inclusion, and other relevant d
Externí odkaz:
https://doaj.org/article/9d68419c5e2e44b5afa04822ff77ed62
Autor:
Douzhong Zhang, Kongquan Chen, Jiguang Tang, Ming Liu, Peixian Zhang, Guisong He, Jun Cai, Xiusong Tuo
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
The in-situ stress and formation pressure are important parameters in shale gas development. They directly affect the well wall stability, the direction of horizontal well drilling, and the fracturing effect during the shale gas development process.
Externí odkaz:
https://doaj.org/article/caf39ce413004666a80932a3e579447d
Publikováno v:
地质科技通报, Vol 40, Iss 5, Pp 11-21 (2021)
Since the gas generation of Lower Paleozoic marine shale, it has suffered from strong structural transformation, resulting in complex enrichment law of shale gas in Nanchuan area. In order to reveal the constraints of Mesozoic and Cenozoic tectonic d
Externí odkaz:
https://doaj.org/article/dbdf6d264d594b0b81078ae935b8e880
Autor:
Douzhong Zhang, Jiguang Tang, Kongquan Chen, Kaiming Wang, Peixian Zhang, Guisong He, Xiusong Tuo
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Shale is a low-porosity and low-permeability reservoir, and structural fractures are the main controlling factor for the migration and accumulation of shale gas. Moreover, tectonic fractures are controlled by the paleo-tectonic stress field. In this
Externí odkaz:
https://doaj.org/article/b2fd338027da445aadb9f22d720f3c33
Publikováno v:
ACS omega. 7(33)
The main types of diagenesis, diagenetic minerals and their formation time sequence in the Ordovician ultradeep (7000 m total depth) carbonate reservoir represented by the Yingshan and Penglaiba Formations (well Tashen-6, Tahe Oilfied, Tarim Basin),
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::71610abcdc88ae2927a1935612c4a48d
https://pubmed.ncbi.nlm.nih.gov/36033658
https://pubmed.ncbi.nlm.nih.gov/36033658
Publikováno v:
Petroleum Exploration and Development, Vol 40, Iss 6, Pp 722-730 (2013)
Based on the research of unconformity type and distribution, and restoration of structural feature of paleo-uplift in the late sedimentary period of Sinian Dengying Formation, the evolution of paleokarst landform and karstic hydrodynamic field during
Externí odkaz:
https://doaj.org/article/9b3c0c59ab5c470b8be81230287715ec
Publikováno v:
SSRN Electronic Journal.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ed0a442915f1c09248e53ad1c1795622
https://doi.org/10.2139/ssrn.4173687
https://doi.org/10.2139/ssrn.4173687
Publikováno v:
Arabian Journal of Geosciences. 14
The Upper Cretaceous Qingshankou (K2n) and Nenjiang (K2q) shale oil from the Changling Sag (CLS) of the Southern Songliao Basin located in NE China was studied to determine shale reservoir properties and evaluate oil potential. Multiple methods, incl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9a1e3797b86bfbbf81d000b46f5761b
https://doi.org/10.1007/s12517-021-07064-9
https://doi.org/10.1007/s12517-021-07064-9
Publikováno v:
Marine and Petroleum Geology. 124:104787
Organic rich Wufeng-Longmaxi shales (WLS) occur widely in the Upper Ordovician–Lower Silurian strata in southeastern Sichuan Basin, SW China. However, complex structural deformation and faulting activity in this area since the Mesozoic time has had
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::938c1f9b10caad2deec806591b0b9eb9
https://doi.org/10.1016/j.marpetgeo.2020.104787
https://doi.org/10.1016/j.marpetgeo.2020.104787
Publikováno v:
International Journal of Coal Geology. 228:103557
One of the biggest challenges in evaluating the transport and storage properties of shales is understanding how the pore structure and network evolve in the same stratigraphic shale during catagenesis. Using a combination of CO2 adsorption, mercury i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::38dcae83652ed451b6ea0eb1296e4453
https://doi.org/10.1016/j.coal.2020.103557
https://doi.org/10.1016/j.coal.2020.103557