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Structural characteristics of the northern Longmenshan fold-thrust belt and the favorable exploration areas, Sichuan Basin, Southwest China

机译:中国西南地区四川盆地龙门山褶皱冲断带北部构造特征及有利勘探区

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Based on the latest data from oil and gas exploration, the structural geometry features of the northern Longmenshan fold-thrust belt and its forming process were examined, and then favorable hydrocarbon prospecting areas were predicted. Two major orogenic events occurred in the Longmenshan belt since the Mesozoic: thrusts and folds were formed by a late Triassic compressional event, and later transformed by the late Cenozoic deformation featuring base-involved large folds. Due to the influence of the two events, thrust nappes, autochthonous thrusts and in-situ blind thrusts developed from the orogen to the foreland basin sequentially, and these structural units show different profile combination from the north to south. Among these structural units, the autochthonous thrusts and folds under lower allochthonous nappes have high potential for oil and gas exploration.
机译:根据油气勘探的最新数据,研究了北龙门山褶皱冲断带的构造几何特征及其形成过程,进而预测了有利的油气勘探区。自中生代以来,龙门山带发生了两个主要的造山活动:逆冲和褶皱是由三叠纪晚期的一次压缩事件形成的,后来又由新生代晚期的变形所转化,其特征是基底卷入的大褶皱。由于这两个事件的影响,冲动推覆,自生冲断和原位盲冲从造山带向前陆盆地依次发展,这些构造单元从北向南呈现出不同的剖面组合。在这些结构单元中,下部异质尿布下的自生推力和褶皱具有油气勘探的巨大潜力。

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