Reservoir Quality and Controlling Mechanism of the Upper Paleogene Fine-Grained Sandstones in Lacustrine Basin in the Hinterlands of Northern Qaidam Basin, NW China
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12583-022-1701-6.pdf
Reference90 articles.
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2. Barth, T., Bjørlykke, K., 1993. Organic Acids from Source Rock Maturation: Generation Potentials, Transport Mechanisms and Relevance for Mineral Diagenesis. Applied Geochemistry, 8(4): 325–337. https://doi.org/10.1016/0883-2927(93)90002-x
3. Baruch, E. T., Kennedy, M. J., Löhr, S. C., et al., 2015. Feldspar Dissolution-Enhanced Porosity in Paleoproterozoic Shale Reservoir Facies from the Barney Creek Formation (McArthur Basin, Australia). AAPG Bulletin, 99(9): 1745–1770. https://doi.org/10.1306/04061514181
4. Bentley, R. W., 2002. Global Oil & Gas Depletion: An Overview. Energy Policy, 30(3): 189–205. https://doi.org/10.1016/s0301-4215(01)00144-6
5. Bethke, C. M., Altaner, S. P., 1986. Layer-by-Layer Mechanism of Smectite Illitization and Application to a New Rate Law. Clays and Clay Minerals, 34(2): 136–145. https://doi.org/10.1346/ccmn.1986.0340204
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