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  nappe
     The Logmenshan thrust nappe belt has been uplifted 5-6km at least since 10Ma B. P., with an uplift rate of more than 0.5-0.6mm/a.
     (2)龙门山逆冲推覆构造带10Ma以来至少隆升了5—6km,隆升速率最低为0.5—0.6mm/a;
短句来源
     (4) The different declination values of Permian, 164°-168° for northwestern and southern margins of Junggar Block,218° for Tarim Block and 229° for Kazakhstan Block, respectively,reveal 35°-55° anticlockwise rotation,probably caused by western nappe structures.
     (4)该地区二叠纪的磁偏角为165°—168°,而塔里木为218°,哈萨克斯坦为229°,说明存在35°—55°的逆时针旋转,这个旋转可能是由于西部推覆构造造成的。
短句来源
     Distribution Characteristics of F02 Fault in Nappe Structure of Xinji Mine Field
     新集井田推覆构造F02断层分布特征
短句来源
     Feasibility study on the relieving mining of seam No.13-1 under nappe structure water-body
     推覆构造水体下13-1煤解放开采可行性研究
短句来源
     The Characteristics and Evolution of Thrust Nappe Structare in the West Margin of Ordos Basin
     鄂尔多斯盆地西缘逆冲推覆构造特征及演化
短句来源
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  napping
     During the study of geological work on the middle segment of Wudang Mountain Nappes the author of this paper discovered six stages of superimposed folds (B_1~B_6). Among them, B_1, B_2, B_3 are folded before the napping, B_4, B_5 are folded during the napping, B_6 is folded after the napping.
     武当山推覆体中段存在六期叠加褶皱(B_1~B_6),其中B_1,B_2,B_3为推覆期前褶皱,B_4,B_5为推覆期褶皱,B_6为推覆期后褶皱。
短句来源
     It possesses the properties of mingle rocks. It underwent the continental napping event at the Suberthem(2000-2400Ma),the amphiboleface metamorphism event at the late Suberthem (1800-2000Ma) and the continental napping event at the late Proterozoic era(600-800Ma).
     它经历了早元古代大陆推覆构造事件(2000~2400Ma)、早元古代末低角闪岩相变质热事件(1800~2000Ma)和元古代末大陆推覆构造事件(6O0~800Ma)。
短句来源
     The strain values range from 22.5—3.7. The total displacement is more than 4.605 km. Various directive stru- ctures indicate that the zone is a compressive-shear ductile shear zone, formed in a napping from north to south.
     整个剪切带呈强、弱应变带相间排列的特征,应变值在22.5~3.7间变化,总位移量大于4.605km,各种指向构造表明该带是由北向南的压剪性推覆型韧性剪切带。
短句来源
     The napping direction goes along SW to NE,the napping distance estimates to be over 100 km and the time should be later than Palaeogene.
     确定其推覆方向是由SW向NE,道冲-推覆距离估计应大于100km。 推覆时代应在早第三纪之后。
短句来源
     The Quaternary source rocks were deposited in the Quaternary depression in eastern basin along with the uplifting of western basin and the strong subsidence of eastern basin during the compressive napping stage.
     挤压、推覆阶段 ,随着盆地西部的隆升 ,东部地区的强烈沉降 ,在盆地东部第四纪坳陷中沉积了第四系烃源岩。
短句来源
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  thrusting nappe
     THE CENOZOIC THRUSTING NAPPE IN NORTHWEST YUNNAN
     滇西北新生代逆冲推覆构造
短句来源
     Mainly based on seismic profile L_(14) and L_(55), the authors discuss the texture, mode, formation time, thrusting distance and oil and gas prospects of the northern sector of thrusting nappe structure of Longmen Mountains.
     本文以L14、L55地震大剖面为主,论述了龙门山逆冲推覆构造带北段的结构、模式、形成期、推覆距及油气远景。
短句来源
     On Geological Texture and Oil and Gas Prospects of the Northem Sector of Thrusting Nappe Structure of Longmen Mountaine
     论龙门山逆冲推覆构造带北段的地质结构及油气远景
短句来源
     (5) back thrusting nappe and foreland decollement as two basic structural patterns;
     (5)背冲推覆和前陆滑脱是两类基本构造样式;
短句来源
     1. The deposition-tectonics evolutionary history in the west margin of Ordos basin include 6 stages: crystalline basement formation stage in the Archaean-Terminal Palaeoproterozoic, stable continental-margin deposition stage in Middle-late Proterozoic-Ordovician, starting stage in the Caledonian thrust nappe structure, marine-continental alternation and inland lake basin formation stage in the late Palaeozoic-Triassic, dominant development stage of the thrust nappe structure in the Jurassic-Neogene period and continuously thrusting nappe stage in the Cenozoic period.
     1、鄂尔多斯西缘6阶段沉积—构造演化历史,包括:太古—古元古代末结晶基底形成阶段、中—新元古代至奥陶纪稳定大陆边缘沉积阶段、加里东运动逆冲推覆构造启动阶段、晚古生代—三叠纪海陆交替和陆内湖盆形成阶段、侏罗纪—新近纪逆冲推覆构造主要发展阶段和新生代持续逆冲推覆阶段。
短句来源
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  “推覆”译为未确定词的双语例句
     The minimal displacement and average rate of southward overthrusting are estimated to be ~30-35 km and 2.4-2.8 mm/a respectively.
     估算最小逆冲推覆距离为30~35km,最小逆冲推覆运动速率为2.4~2.8mm/a。
短句来源
     The formation age of the thrust-imbricate and klippen structures is from the last stage of Palaeozoic to Cenozoic , with determined isotopic age values of mylonite 179 Ma, 149 Ma, 146Ma, 15. 45 Ma and 25. 55 Ma.
     冲断叠瓦构造和推覆构造形成的时代为自古生代末至新生代,已获糜棱岩同位素年龄有179Ma、149Ma、146Ma、15.43Ma和25.55Ma。
短句来源
     Three samples of rocks of different ages in the strong strain belts give K-Ar ages of 155 to 158 Ma,suggesting that the age of the thrust shear is terminal Middle Jurassic.
     强应变带内三件不同时代岩石的K Ar同位素年龄为155~158Ma,表明推覆剪切时代为中侏罗世末。
短句来源
     Application of Both Modified Newton-Raphson Iteration and Arc-Length Method to Pushover Analysis of Building Structures
     修正Newton-Raphson方法和弧长法在结构推覆分析中的联合应用
短句来源
     Capacity spectra of A-D format aregained by means of static push-over method and the method of transforming a multi-degree of freedom system into a single-degree of freedom system.
     能力谱方法的分析步骤:利用R—μ关系基于抗震规范弹性反应谱建立了能力谱方法中的需求谱,利用push-over 推覆分析和将多自由的结构体系转化为等效的单自由度体系的方法得到A-D 格式的能力谱。
短句来源
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  nappe
The thrust-nappe strength of the Qinling-Dabie orogenic belt fault system showed the tendency that the strength was greater in the south and east, but weaker in the north and west.
      
On the contrary, the thrust-nappe strength was greater in the north and west, weaker in the south and east during the late Yanshanian epoch-early Himalayan epoch.
      
The Daba Mountains can be divided into two structural belts by the NW-striking Chengkou fault, namely the northern Dabashan thrust-nappe belt and the southern Dabashan foreland fold-and-thrust belt.
      
The stratotype Chupa Sequence, which makes up the synonymous tectonic nappe and is a member of oldest (Late Archean) rocks in the Belomorian Mobile Belt, is scrutinized.
      
The nappe is mainly composed of the migmatized, coarse-grained garnet-biotite gneiss with kyanite.
      
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  napping
Treatment, which includes counseling, scheduled napping, and pharmacologic intervention, is effective for most patients.
      
Daytime napping and its effects on alertness and short-term memory performance in shiftworkers
      
Daytime napping and its effects on 145 female shiftworkers were studied by comparing the individual characteristics, alertness, and short-term memory performance of subjects who took or did not take naps.
      
After a morning shift, napping was more frequent among evening types and subjects living alone (not married).
      
Before a night shift, daytime napping was not connected to individual characteristics, but the total sleep time of nappers during the preceding night was shorter than that of non-nappers.
      
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The nappe structure in Peng-Guan area, western Sichuan Basin is discussed.The Allochthon consists mainly of Devonian, Permian, Triassic and Protero-zoic rocks which constitutes a klippe group. The autochthonous system includesupper Triassic and Jurassic rocks and forms NE-fold system. The Beichuan-Baoxing fault, which is supposed to be the root zone of the nappe, is char-acterised in strong compression and multistage activation. The nappe structurecompleted its formation during the Himalayan movement when this...

The nappe structure in Peng-Guan area, western Sichuan Basin is discussed.The Allochthon consists mainly of Devonian, Permian, Triassic and Protero-zoic rocks which constitutes a klippe group. The autochthonous system includesupper Triassic and Jurassic rocks and forms NE-fold system. The Beichuan-Baoxing fault, which is supposed to be the root zone of the nappe, is char-acterised in strong compression and multistage activation. The nappe structurecompleted its formation during the Himalayan movement when this fault zoneactivated once more. The leading factor for the nappe structure development ishorizontal compression, while gravitation is only of secondary importance.

本文讨论四川盆地西部彭县、灌县地区的推覆构造。其外来系统主要由泥盆系、二叠系、三叠系及元古代岩体组成,构成飞来峰群。原地系统由上三叠统及侏罗系组成北东向的褶皱系。根带是北川一宝兴断裂带,该断裂带挤压强烈,多期活动,在喜山期再度活动形成推覆构造。该推覆构造形成的主导因素是水平挤压,而重力仅居次要地位。

The northeastern part of the fault zone in Longmen Mountains is a compress-torsional overthrust zone developed from the transition zone between the geosyncline and the massif. It is composed of three nappes and a buried zone, in which the Tianjingshan anticlinorium nappe and the lower wall buried block of Jianyou-Guangyuan fault are the best in oil and gas prospect. There are three kinds of favourable anticline traps in this region where oil and gas seepages appear everywhere, oil and gas resources are abundant...

The northeastern part of the fault zone in Longmen Mountains is a compress-torsional overthrust zone developed from the transition zone between the geosyncline and the massif. It is composed of three nappes and a buried zone, in which the Tianjingshan anticlinorium nappe and the lower wall buried block of Jianyou-Guangyuan fault are the best in oil and gas prospect. There are three kinds of favourable anticline traps in this region where oil and gas seepages appear everywhere, oil and gas resources are abundant and exist three sets of good reservoirs, therefore it is an oil and gas bearing region with good prospect.

龙门山断裂带东北段是由地槽和地块的过渡带发展起来的压扭性逆掩断裂带。它由三个推覆体和一个隐伏带组成,以天井山复背斜推覆体和江油至广元断层下盘隐伏体的含油气远景最好。区内发育三种有利的背斜圈闭,油气苗普遍,油气源丰富,并有三套较好的储层.是一个有良好前景的含油气区。

One interesting fact is that there are several tectonic phcnomena, for instance, the major northeast structures, the arcuate structure in the nortnern edge, the thrust-nappes, the structural belts appearing to be regular chang from northwest to southeast, in this border area. We propose it could be resultec from gravity gliding. During the later Triassic the Jiangnan rise and the Kuenjia anticline in southeastern uplifted. Meanwhile the lower Yangzi sycline in northwestern went down relatively. The sedimentary...

One interesting fact is that there are several tectonic phcnomena, for instance, the major northeast structures, the arcuate structure in the nortnern edge, the thrust-nappes, the structural belts appearing to be regular chang from northwest to southeast, in this border area. We propose it could be resultec from gravity gliding. During the later Triassic the Jiangnan rise and the Kuenjia anticline in southeastern uplifted. Meanwhile the lower Yangzi sycline in northwestern went down relatively. The sedimentary covering layers formed in dipping toward to northwest. It provided a important slope condition for gravity sliding at Yingzhi stage. The gravitational forces drove the rocks masses moving along dipping slope surface from southeast to northwest. The front of gliding rocks masses was resisted near Yangzi river area and was compressed to form the tilting folds and thrusts, and constructed a arcuate strueture. The rear of gliding rocks masses formed the extentional faults and became a eroded area due to extentional effect in the northern Zhejiang area. At Yianshan stage, the basementfaulte were developed.The rocks masses were uplifted and dipped due to faultbloke movement. It gave a new slope condition for gravity sliding at that time. The regular distributions of the structures which were made by gravity gliding provid a structural imformation for searching of oil and gas in this area.

本区主要发育北东向构造,其北缘弧形构造的存在;逆掩断层、推覆体普遍发育;构造变形自西北至东南出现明显的分带性,成为主要的构造特征。综合研究区内的构造特征及其形成的构造背景后,作者认为主要构造是重力滑的产物。晚三叠世、东南的“江南隆起”、昆嘉大背斜较大幅度地上升,西北的下扬子大向斜相对下降,形成沉积盖层向北西倾斜的产状,为印支期重力滑动提供重要的坡度条件。在其他地质因素配合下,重力驱使岩石层沿斜面由东南向西北滑动。滑动岩石层的前锋在长江一带受阻发生强烈挤压,产生紧闭褶皱、逆掩断层,并构成弧形构造;尾端,由于拉张作用而在浙北地区形成北东向的张性断裂和构造剥蚀带。燕山期,基底断裂发育,块断升降造成岩块的抬升、掀斜为这个时期的重力滑动提供了新的坡度条件,导致了推覆体的发育。重力滑动塑造的构造在空间上有规律的布局为本区寻找油气藏提供了构造依据。

 
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