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- W2364025513 abstract "During the Late Permian Changhsingian Stage-Early Triassic Induan Stage, a series of NW-trending deep-water rift basins formed along the northwestern margin of Yangtze block,which are named as the Kaijiang-Liangping rift, the Chengkou-Exi rift and the Jinmen-Dangyang rift respectively from west to east. They are approximately parallel to each other, but perpendicular or sub-perpendicular to the strike of the South Qinling orogen to the north. Giant gas field has been discovered along the edges of the Kaijiang-Liangping rift, which draws broad attention to these rift basins from geologists and oil gas explorers. In this paper, we study the distribution and formation mechanism of these rift systems which have good prospect in oil gas exploration, and indicate that they were collision rifts forming during the closure of the south Qinling Ocean by the initial contact between the Yangtze block and the South Qinling orogen." @default.
- W2364025513 created "2016-06-24" @default.
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- W2364025513 date "2011-01-01" @default.
- W2364025513 modified "2023-09-25" @default.
- W2364025513 title "Distribution and origin of the Late Paleozoic-Mesozoic rift systems in the northern margin of the Yangtze block" @default.
- W2364025513 hasPublicationYear "2011" @default.
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