• The overthrust belt at the south edge of Santanghu basin is the main exploration target.

    南缘逆掩推覆带是三塘湖盆地油气勘探的主攻区带之一。

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  • Depending on the intensity of the deforming forces the folds may be gentle sharp overturned or overthrust.

    根据变形力的强度,褶皱可以是平缓的,陡峭的,倒转的,或逆掩的。

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  • Nitrogen injection being used to enhance oil recovery in many oilfields, particularly in overthrust fault.

    许多油田,特别是在逆掩断层油藏中,正在大量注氮提高原油采收率。

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  • However, the accident of drill string damage happened easily in the overthrust nappe belt of these regions in the drilling.

    但是,在其逆掩推覆带钻井作业中,极易发生钻具失效事故。

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  • The overthrust tectonics at the end of Paleogene are related to the remote effect of subduction of Indian plate beneath Eurasian plate.

    古近纪末期逆冲构造形成机制与印度板块向欧亚板块之下俯冲的远程效应有关。

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  • The left-lateral strike-slip movement of the Zhongwei fault zone since late Pleistocene caused the differentiation of preexisting overthrust faults in the zone.

    青藏高原东北缘的中卫断裂带在晚更新世以来的左旋走滑运动中,先存的挤压逆掩、逆冲断裂带发生了分化。

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  • These thrusts have their special thu- rsting features, being different from the well-known overthrust belt in the premountain regions of Rocky and Alps mountains.

    这些冲断构造不同于常说的落基山、阿尔卑斯山的山前冲断推覆构造,而具有独特的冲断形式。

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  • The overthrust fault zone and foreland basin in Southwestern Tarim is favorable areas for petroleum exploration. But the research and exploration degree here are still low.

    塔西南山前冲断带及其前陆盆地系统是一个油气勘探前景较好的地区,但目前对该地区的研究程度和勘探程度都比较低。

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  • The structural system of nappe consists of several overthrust fracture belts, thrust sheets and thrust slices, and master fault and secondary fault form an imbricate structure.

    推覆构造体系是由几条逆冲断裂带及其逆冲席、逆冲片组成,主干断层与次级断层组成叠瓦式构造。

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  • In present gravity exploration of overthrust nappe, people usually use gravity continuation method, forward gravity modelling method and integrated gravity-seismic interpretation method.

    目前,应用重力资料研究逆冲推覆构造,多采用重力延拓法、重力模型正演法和重力、地震综合解释法。

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  • A large-scale Late Cenozoic overthrust system has been found in the southern East Kunlun Mountains through tectonic mapping and geological reconnaissance in the Dongdatan-East Wenquan area.

    通过对东大滩—东温泉地区的路线地质观测与构造填图,在东昆仑南部发现晚新生代大型逆冲推覆构造系统。

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  • A large-scale Late Cenozoic overthrust system has been found in the southern East Kunlun Mountains through tectonic mapping and geological reconnaissance in the Dongdatan-East Wenquan area.

    通过对东大滩—东温泉地区的路线地质观测与构造填图,在东昆仑南部发现晚新生代大型逆冲推覆构造系统。

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