Abstract
To evaluate source rocks, their quality and quantity must be known. Quality mainly refers to various organic geochemical parameters, while quantity refers to volume, thickness, distribution, as well as the quantity of hydrocarbon generation and accumulation. It is possible to study only the quality and quantity of source rocks in the Mesozoic and Cenozoic basins with non-cyclic evolution in China. For the Mesozoic and Paleozoic multiple cyclic (residual) basins in China, it may not be sufficient to simply study the quality and quantity of source rocks. To confirm the availability of source rocks and quantitatively evaluate their hydrocarbon resources, the accumulation evolution of basins and their current preservation conditions should also be considered.
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References
Cai K, Wang Y, Yang Y et al (2003) Evaluation of hydrocarbon source rocks in Permian and Triassic at Guangyuan-Wangcang region in Northwest Sichuan Basin and a primary discussion on gas source. Nat Gas Ind 23(2):9–15
Dong D, Zou C, Yang H et al (2012) Progress and prospects of shale gas exploration and development in China. Acta Petrolei Sinica 33(S1):107–114
Fang J, Liu B, Jin F et al (2002) Source potential for generating hydrocarbon and exploration prospects of Middle-Upper Proterozoic in the northern China. Acta Petrolei Sinica 23(4):18–23
Guo X, Dongfeng H, Wen Z et al (2014) Major factors controlling the accumulation and high productivity in marine shale gas in the Lower Paleozoic of Sichuan Basin and its periphery: a case study of the Wufeng-Longmaxi formation of Jiaoshiba area. Chinese Geol 41(03):893–901
Huang J, Zou C, Li J et al (2012) Shale gas generation and potential of the Lower Cambrian Qiongzhusi Formation in Southern Sichuan Basin China. Pet Explor Dev 39(1):69–75
Jing T, Yang G, Tuo LIN et al (2015) Geological characteristics and prospective zone prediction of Meso- Epiproterozoic Shale Gas in China. Special Oil Gas Reserv 22(6):5–11
Li Y, Li J (2010) Exploration Prospects of Shale Gas of Upper Sinian-Silurian in Mid-Yangtze Region. Xinjiang Petroleum Geology 31(6):659–663
Li S, Xiao K, Wo J et al (2008) Developmental Controlling Factors of Upper Ordovician-Lower Silurian High Quality Source Rocks in Marine Sequence. South China. Acta Sedimentologica Sinica 26(5):872–880
Li T, He Z, He S et al (2013) Characteristics and its petroleum geological significance of the permian Paleo- Oil reservoir of Jingshan area, the north edge of the central Yangtze block. J Jilin Unv: Earth Sci Edn 43(06):1740–1752
Liang D, Guo T, Chen J et al (2008) Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions, southern China (part 1): distribution of four suits of regional marine source rocks. Marine Origin Pet Geol 13(02):1–16
Liang D, Guo T, Chen J et al (2009) Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions, southern China (part 2): geochemical characteristics of four suits of regional marine source rocks South China. Marine Origin Pet Geol 14(01):1–15
Liu D, Xie Z, Li J et al (2013) The inorganic microelement characteristics and hydrocarbon potential prediction of algal dolomite in Dengying formation from Sichuan Basin. Sci Technol Eng 13(10):2791–2798
Song N, Yang S, Hou P et al (2013) Geological conditions of shale gas in the Wufeng-Gaojiabian formations in lower Yangtze area. Sci Technol Rev 31(33):42–46
Teng G, Qin J, Zheng L (2008) Spatiotemporal distribution of Sinian-Permian excellent marine source rocks in southeastern Guizhou Province. Marine Origin Pet Geol 13(2):37–44
Wang J, Chen D, Wang Q (2007) Platform evolution and marine source rock deposition during the terminal Sinian to early cambRian in the middle Yangtze region. Acta Geol Sin 81(8):1102–1112
Wang S, Chen G, Dong D et al (2009) Accumulation conditions and exploitation prospect of shale gas in the Lower Paleozoic Sichuan basin. Nat Gas Ind 29(5):51–58
Wei G, Xie Z, Song J et al (2015) Features and origin of natural gas in the Sinian-Cambrian of central Sichuan paleo-uplift, Sichuan Basin SW China. Pet Explor Dev 42(06):702–711
Wu H, Yao S, Jiao K (2013) Shale-gas exploration prospect of Longtan Formation in the Lower Yangtze area of China. J China Coal Soc 38(5):870–877
Xia M, Wen L, Wang Y et al (2010) High-quality source rocks in trough facies of Upper Permian Dalong Formation of Sichuan Basin. Pet Explor Dev 37(06):654–662
Yang P, Xie Y, Li X et al (2012) Hydrocarbon-generating potential of the source rocks of the Sinian Doushantuo Formation on the western side of the Xuefeng Mountain. Chinese Geol 39(05):1299–1310
Yong Z, Zhang X, Deng H (2012) Differences about organic matter enrichment in the shale section of Ediacaran Doushantuo Formation in West Hubei of China. J Chengdu Univ Technol: Sci Technol Ed 39(6):567–573
Zhang Y, Zhang B, Wang F et al (2001) Two sets of marine shoveling source beds in Tarim Basin -1. Properties, development environment and control factors of organic matter. Progress Nat Sci 11(03):39–46
Zhang C, Liu G, Zeng H et al (2012) Depositional environments and controlling factors of Permian source rocks in Western Sichuan Basin. Nat Gas Geosci 23(4):626–632
Zhou H (1990) On the mechanism and the characteristics of early Cambrian ‘stone coal’ in lower yangtze region and their relation to petroliferous potentials. Pet Geol Exp 12(1):36–42
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Ma, Y. (2020). Major Source Rocks and Distribution. In: Marine Oil and Gas Exploration in China. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-61147-0_3
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DOI: https://doi.org/10.1007/978-3-662-61147-0_3
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