2022
DOI: 10.1016/s1876-3804(22)60019-3
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Silurian hydrocarbon exploration breakthrough and its implications in the Shajingzi structural belt of Tarim Basin, NW China

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Cited by 8 publications
(10 citation statements)
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“…The Shajingzi Belt is located in the southeast of Wensu salient, which is classified as the secondary tectonic unit in the northwest Tarim Basin and belongs to a typical basin-range junction belt (Zhang et al, 2022). It strikes in the northeast-southwest direction and was defined mainly by three boundary faults including the Karayuergun Fault in the north, the Yingan Fault in the south, and the Shajingzi Fault in the southeast, respectively (Figure 1A-C).…”
Section: Geological Settingmentioning
confidence: 99%
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“…The Shajingzi Belt is located in the southeast of Wensu salient, which is classified as the secondary tectonic unit in the northwest Tarim Basin and belongs to a typical basin-range junction belt (Zhang et al, 2022). It strikes in the northeast-southwest direction and was defined mainly by three boundary faults including the Karayuergun Fault in the north, the Yingan Fault in the south, and the Shajingzi Fault in the southeast, respectively (Figure 1A-C).…”
Section: Geological Settingmentioning
confidence: 99%
“…It strikes in the northeast-southwest direction and was defined mainly by three boundary faults including the Karayuergun Fault in the north, the Yingan Fault in the south, and the Shajingzi Fault in the southeast, respectively (Figure 1A-C). The Shajingzi Fault accompanied with numerous secondary faults is regarded as the boundary between the Wensu Salient and the Awati Sag (Jia, 2005;Wang et al, 2009;Li et al, 2013;Qi et al, 2014;Zhang et al, 2022) (Figure 1C). Approximately, the fracture systems involve deep wedge-shaped thrusts, Shajingzi Fault in a narrow sense (painted in Figure 2), and shallow extensional faults as a whole (Li et al, 2013;Qi et al, 2014;Zhang et al, 2022).…”
Section: Geological Settingmentioning
confidence: 99%
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