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Titlebook: Marine Oil and Gas Exploration in China; Yongsheng Ma Book 2020 Geological Publishing House and Springer-Verlag GmbH Germany 2020 Explorat

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Major Source Rocks and Distributionfers 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 (r
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Reservoir Type and Spatial Distributionre are more than 20 stable continental masses in China and are characterized by a small area. The largest continental mass is the North China Craton with an area of ~170 × 10. km.. The total area of the stable continental masses is ~455 × 10. km.. Compared with the huge cratons in North America and
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An’yue Gas FieldGaoshiti–Longnvsi tectonic group in the gentle structural zone of the Central Sichuan paleo-uplift, Sichuan Basin. The gas field is adjacent to the Guang’an structure in the east, Weiyuan anticline and Ziyang ancient trap in the west, Penglaizhen structure in the north, and Hebaochang structure and
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Progress and Theory of Marine Strata Oil and Gas Exploration in the Ordos BasinFig. 13.1). The structural configuration of the basin is clear. It is surrounded by massive mountains including the Yinshan, Qinlin, Lvliang, and Helanshan in the north, south, east, and west, respectively. The margin of the basin was rounded by large rivers such as the Yellow and Wei Rivers. The no
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Daniudi Gas Fieldr, Inner Mongolia Autonomous Region (Fig. 15.1) with the geographic coordinates of 109°30ʹE–110°00ʹE and 38°45ʹN–39°10ʹN (Wang 2012). The gas field is located in the eastern part of the Maowusu Desert. The terrain is relatively flat. The ground is covered with sand and dunes, and the height of the d
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Regional Tectonic Setting and Prototype Basin Evolutiond among them (Ren and Huang in Tectonics and their evolution in China: 1: 4 million tectonic maps of China. Science Publishing House, Beijing, .; Li in Principal characteristics of the lithosphere of China. Earth Sci Front 17(3):001–013, .).
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