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1)  Bogeda overriding tectonics
博格达推覆构造
2)  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
3)  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。
4)  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。
5)  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。
6)  thrust nappe structure
推覆构造
1.
The nappe structures in the area are formed in the late Cretaceous and may be divided into 4 deformable zones,namely,imbricated thrust nappe structure zone,closed folded-thrust faulted deformable zone,wide-gentle folded-faulted turned folded zone and decollement folded-faul.
它主要由韧性剪切带、韧脆性剪切带和推覆构造等构成。
2.
The North Wuyi area is characterized by advantageous mineralizing geological conditions and widespread mineral resources, but the formation and conservation of ore deposits are mainly controlled by thrust nappe structure.
北武夷地区成矿地质条件优越,矿产资源分布广泛,而广泛发育的推覆构造深刻影响着矿床的成生与保存。
补充资料:调达推山
【调达推山】
  佛往昔于罗阅只城,有长者名须檀,家富多财,子名须摩提。其父须檀命终已后,摩提异母弟名修耶舍摩提,不欲与弟分财。一日与弟执手,共登耆阇崛山,将至高崖,便推置崖底,以石塠之,其弟命绝。佛告舍利弗:长者须檀者,我父王白净是也。须摩提者,则我身是。修耶舍者,今提婆达多是也。以是因缘,我于耆阇崛山经行,为提婆达多举崖石以掷我头,山神以手接石,石边小片,迸中我脚,拇指破而血出。(梵语耆阇崛,华言鹫头,即灵鹫山也。须檀、须摩提俱无翻。)
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