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The Ordos Basin in the western part of the North China Craton is commonly believed to be a multi-controlled oilbearing basin.It is bounded by the Xing’an-Mongolian Orogen to the north,the Qingling Orogen to the south,the Lüliang mountain to the east and the Helanshan-Liupanshan mountain belt to the west.The interpretation of geophysical data reveals a latitudinal(38°)fault belt in the centre of the Ordos Basin,which controls the hydrocarbon generation,migration and accumulation in the basin.This study attempts to
The Ordos Basin in the western part of the North China Craton is commonly believed to be a multi-controlled oilbearing basin. It is bounded by the Xing’an-Mongolian Orogen to the north, the Qingling Orogen to the south, the Lüliang mountain to the east and the Helanshan-Liupanshan mountain belt to the west. The interpretation of geophysical data reveals a latitudinal (38 °) fault belt in the center of the Ordos Basin, which controls the hydrocarbon generation, migration and accumulation in the basin. This study attempts to