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《Geotectonica Et Metallogenia》 1985-02
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TECTONIC EVOLUTION OF THE ERLIAN BASIN AND ITS BEARING ON OIL AND GAS

FEI Baosheng (Research Institute of North China for Petroleum Exploration and Exploitation)  
The Erlian Basin has two basic structural layers: geosynclinal, the basement, and diwa, the cover. The cover is divided into three sublayers. It contains rich resources of oil and gas.The Erlian Basin is extensional in nature, has all kinds of trap types and consists of many uplifts and depressions.Magmatic activities occurred several times, resulting in a high-geothermal gradient favorable for oil-gas transformation.The specific feature of the tectonic evolution of the Ertian Basin is that it underwent a geosynclinal stage in the Paleozoic and a diwa stage in the Mesozoic, without a platform stage in between. The diwa stage underwent three periods, swelling (T) and fault-depression (J_(1-2)); faulting-folding (J_3); and fault-depression and block-faulting (K_2—Q). The author suggests that the NE-trending depression is favourable for exploration and that multiple accumulation zones of oil and gas can occur along large faults. The author also applies the theory of progression of metallogenesis to oil exploration. It is suggested that the geosynclinal structural layer is a promising site for the search for all types of buried hill oil Pools; the diwa structural layer, oil pools originated and reserved within itself or originated below and reserved above.In addtion, the strong crustal movement and high geothermal gradient in the region are favourable for the formation of coal gas.
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