2021
DOI: 10.1007/s13369-021-05863-6
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Characteristics and Forming Processes of Reef-Shoal Reservoir in Changhsing Formation of the Eastern Sichuan Basin in Dianjiang, China

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“…The Ordovician began to water-transgress, and the Sichuan Basin was dominated by shelfto-basin facies. At the end of the Silurian, the Late Caledonian movement came the uplift and denudation of the Leshan-Longnusi paleo-uplift, resulting in an angular unconformity between the Cambrian and Permian strata in the southwestern Sichuan Basin (Su et al, 2020;Luo et al, 2022). The Xixiangchi Formation in the Southwestern Sichuan Basin is denuded (Gu et al, 2020;Li et al, 2020) (Figure 1B).…”
Section: Geological Settingmentioning
confidence: 99%
“…The Ordovician began to water-transgress, and the Sichuan Basin was dominated by shelfto-basin facies. At the end of the Silurian, the Late Caledonian movement came the uplift and denudation of the Leshan-Longnusi paleo-uplift, resulting in an angular unconformity between the Cambrian and Permian strata in the southwestern Sichuan Basin (Su et al, 2020;Luo et al, 2022). The Xixiangchi Formation in the Southwestern Sichuan Basin is denuded (Gu et al, 2020;Li et al, 2020) (Figure 1B).…”
Section: Geological Settingmentioning
confidence: 99%