1) Giant Nappe Structure
巨型推覆构造
1.
Research on Giant Nappe Structure and Golden Deposit Prediction in North of Heilongjiang Province;
黑龙江省北部巨型推覆构造和金矿预测
3) nappe structure
推覆构造
1.
A discussion on nappe structure pattern in the jiu mountains and the south of the lower reaches of the changjiang river by the remote sensing image;
根据遥感影像讨论九岭──江南地区的推覆构造格局
2.
Latest Permian-earliest Triassic nappe structure in the Ulan Haya area on the northern margin of the North China platform;
华北地台北缘乌兰哈雅地区二叠纪末—三叠纪初推覆构造
3.
Discovery and significance of nappe structure in Yucheng area.
禹城地区推覆构造的发现及意义
4) nappe
[英][næp] [美][næp]
推覆构造
1.
On the basis of analysing the structural features and the genetic mechanism of nappe, gliding nappe and fault-block structures in Linru Coalfield, Hexichen, Wenquan Street and the deep part of Chaochuan mining area are considered as the favourable districts for tracing coal.
在分析临汝煤田的推覆构造、滑覆构造及断块构造特征和成因机制的基础上,指出了河西陈、温泉街、朝川矿区深部等找煤的有利区段。
2.
The comprehensive analyses from strata distribution,gravity,geomagnetism,seismic and CEMP data show that the thrust structural belt in western margin of Ordos basin is composed of Liupanshan arc thrust system and Zhuozishan-Helanshan thrust system,which are two independent nappe tectonic systems.
地层分布、重力、磁力、地震、CEMP多种资料综合分析认为,鄂尔多斯盆地西缘冲断构造带由六盘山弧形冲断体系和桌子山-贺兰山冲断体系组成,它们是互为独立的冲断推覆构造;明确指出,六盘山弧形冲断体系为祁连地体拼贴到华北陆缘地体(鄂尔多斯地块西部)之上的冲断推覆构造,具有独特的双层地体叠置结构。
5) thrust
[英][θrʌst] [美][θrʌst]
推覆构造
1.
The northern Qinling margin thrust structural zone in S→N direction is composed of two structural zones which are Yiyang-Lushan fault zone and Xiong er rock sheet.
主要包括秦岭北缘反冲推覆构造带，以宜阳-鲁山断裂带和熊耳岩片为主体，由S→N逆冲推覆，栾川-伏牛山推覆构造带特征典型，分带性强，由N→S推覆；马超营走滑转换构造带位于二者之间，为一正花状构造带。
2.
In the Huaqiao-Dajiangkou area, there are developed a series of imbricated thrust nappes on the foreland faulted belt northwest of the collision zone between the northwestern and central Hunan terrains.
湘西北地体与湘中地体碰撞拼贴带北西侧的前陆冲折带上发育一系列叠瓦状排列的逆冲推覆构造 ,向北西方向推覆 ,具双重逆冲推覆特征。
6) nappe tectonics
推覆构造
1.
Nappe tectonics was classified into three types thrust nappe tectonics, slipping tectonics (stretch nappe tectonics) and tenacity nappe tectonics.
依据推覆构造形成的力学机制，将推覆构造分为边冲推覆构造、滑覆构造和韧性推覆构造三大类型。
补充资料：推覆构造
| 推覆构造 nappe tectonics 由冲断层及其上盘推覆体和下盘组合而成的整体构造。冲断层总体倾斜平缓，常呈上陡下缓的铲状或下陡上缓的倒铲状，也可呈陡、缓相间的台阶状。上盘为由远距离（数千米至上百千米）推移而来的外来岩块，称推覆体。下盘为较少位移的原地岩块。推覆构造多发育于造山带及其前陆地区。 一个大的推覆体 ，沿其逆冲方向可分为根带、中带和前锋带。根带是推覆体的源区，岩石变形强烈，中带为推覆体的主体，由于经受了强烈的挤压和单剪作用，其中岩石常发育有剪切褶皱、劈理及次一级叠瓦状的冲断层。前锋带自由度大，常形成断裂和等厚褶皱。由于构成推覆构造的冲断层面起伏延展，如经后来的剥蚀作用，在前锋带和中带可形成被原地岩块包围的外来岩块孤丘，称飞来峰，以及在外来岩块中暴露出原地岩块天窗，称为构造窗。 |
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参考词条