首页> 外文期刊>Science in China. Series D, Earth sciences >Structural features and petroleum geology of the fold-thrust belt in the southern Tarim basin, China
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Structural features and petroleum geology of the fold-thrust belt in the southern Tarim basin, China

机译:塔里木盆地南部褶皱冲断带的构造特征和石油地质

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摘要

The west Kunlun fold-thrust belt (WKFTB) and the Altun fold-thrust belt (AFTB) are respectively located in the southern margin of the Tarim basin, NW China. The analyses of typical structures and regional dynamics of the fold-thrust belts reveal their different structural and petroleum features and mechanisms. WKFTB differs from AFTB by abundant fault-related folds and triangles zones, and was formed by northward extrusion of the west Kunlun orogen. AFTB was affected synchronously by northward extrusion of the Altun orogen and the sinistral strike-slipping of the Altun Fault, so it is characterized by the minor scale and the monotonous structural styles. The Aqike anticline and the Aqike fault, of which the strikes are orthogonal to the strike of the fold-thrust belts, are regarded as the adjustive structures between both of the fold-thrust belts. The oil-gas pools of WKFTB develop mainly in the faulted-related anticline traps, but the oil-gas pools of AFTB develop mainly in the low fault-block and anticlines traps related with the pa-leo-uplifts. There are different exploration countermeasures for both of the fold-thrust belts.
机译:西昆仑褶皱冲断带(WKFTB)和阿尔敦褶皱冲断带(AFTB)分别位于中国西北塔里木盆地的南缘。褶皱冲断带的典型构造和区域动力学分析表明它们具有不同的构造,石油特征和机理。 WKFTB与AFTB的不同之处在于大量的断层相关褶皱和三角形带,并且是由昆仑造山带西缘向北挤压形成的。 AFTB受到Altun造山带向北挤压和Altun断层的左旋走滑同步影响,因此其特征是规模较小且结构形式单一。走向与褶皱冲断带走向正交的阿奇克背斜和阿奇克断裂被认为是两条褶皱冲断带之间的调整构造。 WKFTB的油气藏主要发育在与断裂有关的背斜圈闭中,而AFTB的油气藏主要发育在与古隆起有关的低断块和背斜圈闭中。这两个褶皱-冲断带都有不同的勘探对策。

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