Mixed carbonate-siliciclastic reservoir characterization and hydrocarbon accumulation process of the Ganchaigou area in the western Qaidam Basin, Tibet Plateau
Author:
Funder
China National Petroleum Corporation Prospective Research Project
PetroChina Science and Technology Innovation Project
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
https://link.springer.com/content/pdf/10.1007/s13146-022-00769-2.pdf
Reference68 articles.
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2. Bush MA, Saylor JE, Horton BK, Nie J (2016) Growth of the Qaidam Basin during cenozoic exhumation in the northern Tibetan Plateau: Inferences from depositional patterns and multiproxy detrital provenance signatures. Lithosphere 8(1):58–82. https://doi.org/10.1130/L449.1
3. Campbell AE (2005) Shelf-geometry response to changes in relative sea level on a mixed carbonate–siliciclastic shelf in the Guyana Basin. Sed Geol 175(1):259–275. https://doi.org/10.1016/j.sedgeo.2004.09.003
4. Cheng F, Jolivet M, Fu S, Fu S, Zhang Q, Guan S, Yu X, Guo Z (2014) Northward growth of the Qimen Tagh range: a new model accounting for the late Neogene strike-slip deformation of the SW Qaidam Basin. Tectonophysics 632:32–47. https://doi.org/10.1016/j.tecto.2014.05.034
5. Cheng F, Guo Z, Jenkins HS, Fu S, Cheng X (2015) Initial rupture and displacement on the Altyn Tagh fault, northern Tibetan Plateau: constraints based on residual Mesozoic to Cenozoic strata in the western Qaidam Basin. Geosphere 11(3):921–942. https://doi.org/10.1130/GES01070.1
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