The thrust nappe is assembled by root zone, major thrust zone and thrust front.
逆冲推覆体由根带、主逆冲带和逆冲传播前缘带三部分组成。
The main type of the west margin tectonics belt of the Ordos massif is characterised by thrust nappe.
鄂尔多斯地块西缘构造带的主要形式是逆冲推覆构造。
The over thrust nappe consists of four parts: nappe system, front zone, outer front zone and autochthon.
逆冲推覆构造由推覆体系、前缘带、前缘外带和原地岩体四部分组成的。
The geochemical gold anomaly areas in south side of the two thrust nappe structure belts are key prospecting for further ore exploration.
金成矿受地层岩性、构造等因素的控制，在金矿床上均有化探金异常。
The over-thrust nappe in the margin of Daba Mountain is a zone with complex structures but fairly good prospects to hydrocarbon exploration.
大巴山前缘逆冲推覆带足一个构造复杂，但油气前景较好的地区。
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的逆冲推覆构造，该逆冲推覆构造形成于晚侏罗世至早白垩世时期。
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和展布格局，特别强调逆冲推覆断裂的重要性；
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为一巨型水电站，库首区发育一逆冲推覆构造——马家河坝断层。
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.
瓦石峡凹陷山前带发育冲断推覆构造，侏罗系烃源岩增厚有利于油气成藏。
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缘和北西缘分布，控制铅锌矿床的就位与分布，为成矿期构造。
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.
盆地早期的构造样式均为半地堑式箕状凹陷，晚期均发生方式不同的的构造反转，形成全反转的逆冲推覆和半反转的正或逆反转构造。
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。
The suprasalt structure includes suprasalt rolling anticline, fault-bending anticline, suprasalt pop-up, thrust screened structure and salt nappe.
盐上构造包括盐上滚动背斜、断弯-断展背斜、背冲断块、逆冲断层遮挡构造和盐推覆构造等；
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.
根据与其它气田构造的对比，穿盐断裂和叠瓦冲断带的构造组合样式对油气的聚集最为有利。
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逆冲推覆构造的主要标志是逆冲叠瓦扇和软弱滑动层的存在。
Studing the thrust-nappe help us to re-establish the Songshugou ophiolite sequence and its ancient tectonic environment.
松树沟逆冲推覆构造研究对恢复蛇绿岩组合层序及其古构造环境具有重要的地质意义。
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.
盐岩层的存在使库车前陆褶皱-冲断带发育-系列盐相关构造，其中最引人注目的是盐推覆构造。
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.
罗城铜矿区处于九岭南缘大型推（滑）覆构造往南突出的前锋与NNE向走滑冲断带复合部位。
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，与扬子、华夏古板块结合带叠加部位。
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.
本文以详实的野外第一性资料，着重阐述了其推、滑覆构造特征，并分析了成因机制。
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.
早石炭世末，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。
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.
对主干逆冲断裂带及其间的逆冲推覆体带、逆冲席带和低应变区的特征进行了详细描述。
The thrust-nappe system is a para autochthone for its little thrust distance.
该套逆冲推覆系统其推覆距离不大，基本上为一套准原地系统。
The main kinds of the nappes are sheet thrust, Jurassian fold nappe, wedge-shaped nappe and shearing fold-thrust structure, etc.
其主要类型有席状逆冲构造、侏罗山式褶皱推覆构造、楔状推覆构造及剪切褶皱逆冲构造等。
The main kinds of the nappes are sheet thrust, Jurassian fold nappe, wedge-shaped nappe and shearing fold-thrust structure, etc.
其主要类型有席状逆冲构造、侏罗山式褶皱推覆构造、楔状推覆构造及剪切褶皱逆冲构造等。
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