• The main type of the west margin tectonics belt of the Ordos massif is characterised by thrust nappe.

    鄂尔多斯地块西构造主要形式逆冲覆构造。

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  • The over thrust nappe consists of four parts: nappe system, front zone, outer front zone and autochthon.

    冲推构造推覆体系前缘、前缘外带原地岩体部分组成

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  • The geochemical gold anomaly areas in south side of the two thrust nappe structure belts are key prospecting for further ore exploration.

    成矿受地层岩性、构造等因素控制,金矿床上均有化探异常

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  • The over-thrust nappe in the margin of Daba Mountain is a zone with complex structures but fairly good prospects to hydrocarbon exploration.

    大巴山前缘逆冲一个构造复杂油气前景好的地区。

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  • Results Large thrust nappe structure was developed along ZW1 seismic survey line, and it was formed during Late Jurassic to Early Cretaceous.

    结果中卫探区ZW 1地震剖面上发育大型冲推构造,逆冲推覆构造形成于侏罗世白垩世时期。

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  • Then, the regional structure characteristics and distribution pattern are analyzed and the importance of thrust nappe fault is emphasized especially.

    然后分析区域构造特征展布格局特别强调逆冲推覆断裂重要性

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  • The Xiluodu Hydropower Station on the Jinsha River is a giant hydropower station, but a thrust nappe structure-Majiahe Dam fault-lies in the reservoir head region.

    金沙江溪洛渡水电站巨型水电站,首区发育一冲推覆构造——马家河坝断层

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  • In the piedmont belt of Washixia sag developed thrust nappe which leaded to incrassation of Jurassic source rocks, being favorable for hydrocarbon accumulation in this area.

    石峡凹陷山前发育冲断推构造,侏罗系烃增厚有利于油气成藏。

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  • Thrust nappe system, extending along southeast and northwest margin of Bajiazi basin. controls the emplacement and distribution of Pb-Zn deposits, so it is metallogenic structure.

    逆冲推覆构造系统沿八家子盆地东北西缘分布控制铅锌矿就位分布,成矿期构造

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  • The structural styles of the basins in early stage are all half-graben depression and in late stage are total-reverse thrust nappe and semi-reverse normal- or abnormal-reverse structures.

    盆地早期构造样式均为半地堑凹陷晚期均发生方式不同的构造反转,形成全反转的冲推覆半反转的正逆反转构造。

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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.

    构造体系冲断裂带及其冲席、组成主干断层次级断层组成叠瓦式构造。

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  • The suprasalt structure includes suprasalt rolling anticline, fault-bending anticline, suprasalt pop-up, thrust screened structure and salt nappe.

    构造包括盐上滚动背斜、断弯-断展背斜、背冲断块、逆冲断层遮挡构造推覆构造等

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  • The most efficient structural assemblage zone for gas accumulation is the thrust fault and nappe thrust belt developed in a variety of salt-related due to tectonic compression and salt flexible fluid.

    根据其它气田构造对比,穿断裂叠瓦冲断构造组合样式油气聚集最为有利

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  • The imbricate fan of thrusts and soft layer are main structure features distinguishing thrust-nappe structure in magma-tic body area.

    野外判定岩浆岩地区冲推覆构造主要标志逆冲叠软弱滑动的存在。

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  • Studing the thrust-nappe help us to re-establish the Songshugou ophiolite sequence and its ancient tectonic environment.

    松树冲推覆构造研究恢复绿岩组合层序及其构造环境具有重要的地质意义。

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  • A variety of salt-related structures have developed in the Kuqa foreland fold-thrust belt, in which the most fascinating structure is the salt nappe complex.

    盐岩层存在使库车前陆褶皱-冲断带发育-系列相关构造其中引人注目盐推覆构造。

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  • The Luochen Copper Mine is situated at the composite part of the protruding south front of the large scale thrust( slip) nappe and the NNE-trend strike-slip thrust fault in the south edge of Jiuling.

    罗城矿区处于九岭南缘大型覆构造突出前锋NNE向走滑冲断带复合部位

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  • North Jiangxi area is located in the superimposed part of foreland nappe thrust zone of the southeast coast of Eurasian Contiental Plate and Yangzi and Precambrian Cathaysia Plates.

    江西北部地处欧亚大陆板块东南沿海前陆推覆冲断带,扬子华夏古板块结合带叠加部位。

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  • This paper mainly deals with the characteristics of the thrust na ppe and sliding nappe structures with detailed field first-hand data and prelim inarily analyzes their genetic mechanism.

    本文详实野外第一性资料,着重阐述了构造特征,并分析了成因机制。

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  • The continental collision between Siberian and Kazakhstan-Junggar in Early Carboniferous shaped the large-scale dual thrust-nappe structures in the Altay orogen, NW China.

    石炭世末,准噶尔-哈萨克斯坦与西伯利亚板块发生陆-陆碰撞形成大型双重逆冲推覆构造。

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  • The main thrust-slip fault belts and the nappe structure zones, thrust sheets and low strain regions lying in between the main thrust-slip fault belts are described in detail.

    主干断裂带及其的逆冲推覆、逆冲席应变区的特征进行了详细描述。

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  • The main kinds of the nappes are sheet thrust, Jurassian fold nappe, wedge-shaped nappe and shearing fold-thrust structure, etc.

    主要类型有席逆冲构造、侏罗山式褶皱构造、楔状构造剪切褶皱冲构造等。

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  • The main kinds of the nappes are sheet thrust, Jurassian fold nappe, wedge-shaped nappe and shearing fold-thrust structure, etc.

    主要类型有席逆冲构造、侏罗山式褶皱构造、楔状构造剪切褶皱冲构造等。

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