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tectonic stacking
相关语句
  构造迭加原理
     APPLICATION OF TECTONIC STACKING IN FOLD QUANTITATIVE CALCULATION
     构造迭加原理在褶皱定量计算中的应用
短句来源
  “tectonic stacking”译为未确定词的双语例句
     Based on thermochronologic analysis and regional tectonic setting as well as other geological data, the authors consider that the lower crust of Wufengxian, Dayishan and Qitianling areas was thickened by 4100~7700m as a result of tectonic stacking in late Middle Triassic, suggesting that there existed violent intracontinental orogeny at the early stage of the Indosinian movement.
     根据热年代学分析结果,结合区域构造背景和其它地质资料,推断五峰仙、大义山、骑田岭等地区在中三叠世后期因构造叠置增厚了4100~7700m以上,证明印支运动早期为强烈的陆内挤压造山运动。
短句来源
  相似匹配句对
     APPLICATION OF TECTONIC STACKING IN FOLD QUANTITATIVE CALCULATION
     构造迭加原理在褶皱定量计算中的应用
短句来源
     ON TECTONIC SYSTEMS
     论构造体系
短句来源
     Criticize and Tectonic
     批判与建构
短句来源
     FRESNEL INTEGRAL AND STACKING
     费涅耳积分与叠加
短句来源
     According to the tectonic features of ore stacking by blasting for in-situ leaching, the three-layer feedforward neural network was established.
     根据原地爆破浸出工艺爆破筑堆的技术特点 ,构建了 3层前馈型神经网络结构。
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  tectonic stacking
These moderate PT conditions prevailed during the main tectonic stacking event (50-37?Ma), prior to the Mio-Pliocene event.
      
The thick and cold East European platform reacted as a stable rigid block which resulted in a narrow zone of intense crustal shortening, tectonic stacking and high strain at its eastern margin.
      
The present configuration and thickness of the orebody is due to the tectonic stacking of a thin and extensive blanket (2-4?km2) of massive sulphides with low aspect ratio.
      
The tectonic stacking, deformation, metamorphism, and granite formation are related to orogenic events that occurred 0.80-0.78 Ga and 0.61-0.59 Ga ago.
      
At the end of the Paleoproterozoic, the volcanic and sedimentary rocks of the Vetreny Belt underwent tectonic stacking as a result of the countermotion of the crystalline masses of the Vodlozero Massif and the Belomorian-Lapland Belt.
      


The Wudang Group, belonging to the sourthern Qinling orogene, is the folded rocks which are composed of the tectonic stacking meta-sedimentary rocks and metavolcanic rocks. It is characterized by layer circle and indicated by the bedding decollemental shear zones in different levels, Which delegate the characteristic of deformation in the pre-In dosinian orogeny. The b-type decollemental shear zones,the ductile-brittle shear zones and brittle shear zones, which are result from the Indosinian orogeny,reflect...

The Wudang Group, belonging to the sourthern Qinling orogene, is the folded rocks which are composed of the tectonic stacking meta-sedimentary rocks and metavolcanic rocks. It is characterized by layer circle and indicated by the bedding decollemental shear zones in different levels, Which delegate the characteristic of deformation in the pre-In dosinian orogeny. The b-type decollemental shear zones,the ductile-brittle shear zones and brittle shear zones, which are result from the Indosinian orogeny,reflect deformational effects in the different developing stages of earth crust in this areas. Finally, the vast Wudang Nappe make out.

位于南秦岭造山带的武当群为构造堆垛的变沉积岩和由变火山岩组成的褶叠岩系,具圈层性变形特征,显示出在分层剪切作用下形成不同层次的顺层滑脱剪切带,代表了印支期前的变形特征。印支期碰撞造山作用产生的b型褶皱和韧—脆性及脆性剪切带,分别反映了该区地壳不同发展时期的变形效应,最终形成武当巨型推覆体。

The northern portion of Sino Korea Craton consists of four independent blocks and each includs several metamorphic terrains or belts Three styles of early Preambrian metamorphic evolution and their PTt D paths have been distinguished in these terrains The first style was found in Jning Huaián Archaean high grade terrain of Inner Mongolia This district is characterized by widespread Al rich para gneiss (Khondalite suite)and some hypersthene plagioclase gneisses of granulite facies They were subiected...

The northern portion of Sino Korea Craton consists of four independent blocks and each includs several metamorphic terrains or belts Three styles of early Preambrian metamorphic evolution and their PTt D paths have been distinguished in these terrains The first style was found in Jning Huaián Archaean high grade terrain of Inner Mongolia This district is characterized by widespread Al rich para gneiss (Khondalite suite)and some hypersthene plagioclase gneisses of granulite facies They were subiected to five episodes of tectonic deformation and six stages of metamorphism from 2 6Ga to 1 9Ga The mineral paregenesis and transformation of Al rich gneisses in the whole process of metamorphism show a trend of Ky Sil+Grt+Bt+Kfs→Crd±Opx→And The metamorphic PTt D path of this terrain is clockwise with T=800℃~850℃,P=0 90GPa~1 00 GPa in its peak stage and a typical isothermel decompression (ITD)process in post peak stage It reflects double thickening of crust by geodyamic process such as A subduction and tectonic stacking in a collisional belt,followed by tectonic thinning and uplifting in the later stage The second style has been established in eastern Hebei western Liaoning Archaean high grade terrain which is mainly composed of late Archaean grey gneiss (TTG intrusions) and other granitic rocks with Subordinate volcano sedimentary supracrustal sequences and some layered basic intrusions The mineral evolation of basic rocks in granulite facies belt is characterized by assemblege of Opx +Cpx +Hb+Grt+pl in its peak metamorphism with T=800~850℃,P=0 70~0 80GPa,and extensive development of Grt corona around Opx or Cpx during its post peak stage All data give rise to a counter clockwise PTt D path with a nearly isobaric cooling process at its post peak stage It indicats the tectonic environment of vertical crustal thickening by magmetic accretion The third style of PTt d path was constructed in eastern Liaoning southern Jilin early Proterozoic metamorphic belt It was a rifted ensialic depression within the Jiao Liao Massif during the middle stage of early Proterozoic with the formation of sedimentary sequences of shallow sea and continental shelf by the end of early Proterozoic,they were subjected to three deformational episodes and five stages of metamorphism with the development progradal zones and a typical thermal anticline Its axial area is characterized by high amphibolite facies metamrorphism The mineralogic evolution in its Al rich rocks is AndSil+Grt+CrdKy Its PTt D loop is also counter clockwise, but it is distinguished from the second style by rapid raising pressure in its early stage and succeeded by a nearly isobaric heating process and lower pressure (0 50~0 60GPa)in peak stage Such PTt D path may be genetically related to the closing process of a rifted depression within a rather stable continental massif

中朝克拉通北部早前寒武纪变质作用演化及其PTt轨迹主要有三类样式:第一类以内蒙古集宁—怀安太古宙高级区为代表,PTt轨迹表现为顺时针形式,峰期温压高达800℃~850℃,0.90GPa~1.00GPa,峰期后为大幅度等热减压,反映了板块碰撞造山带的陆壳成倍构造增厚和后期拉张减薄机制;第二类以冀东—辽西太古宙高级区为代表,PTt为逆时针形式,早期增温为主,峰期温压均较高,峰期后为近等压冷却过程,它们反映地壳因岩浆底侵而增厚的动力学机制;第三类以辽东—吉南早元古代变质地带为代表,PTt轨迹亦为逆时针,但特征是早期增压明显,继之以近等压增温,峰期为中低压,峰期后近等压冷却,这类样式反映了较稳定陆块壳内裂陷区的闭合过程。

Southeast Hunan lies on the margin of central Naning Mountains. Thermochronological dating was used to study the Meso-Cenozoic thermal history and the uplift processes of five plutons in southeast Hunan. Based on regional tectonic settings, the authors probed into the relationship between the thermochronological evolution and the tectonic development. The results show that the Meso-Cenozoic uplift process of southeast Hunan can be divided into 4 stages, developing in order of fairly rapid uplift→rapid uplift→slow...

Southeast Hunan lies on the margin of central Naning Mountains. Thermochronological dating was used to study the Meso-Cenozoic thermal history and the uplift processes of five plutons in southeast Hunan. Based on regional tectonic settings, the authors probed into the relationship between the thermochronological evolution and the tectonic development. The results show that the Meso-Cenozoic uplift process of southeast Hunan can be divided into 4 stages, developing in order of fairly rapid uplift→rapid uplift→slow uplift→rapid uplift, with the fairly rapid uplift process at an average rate of 0.069mm/a during 222~146.4Ma, the rapid uplift process at an average rate of 0.113~0.186mm/a during 146.4~94.11Ma, the slow uplift process at an average rate of 0.014~0.028 mm/a during 94.11~14.8Ma, and the rapid uplift process at an average rate of 0.143~0.295mm/a during 14.8Ma~0.0Ma. The uplift rate speeded up at the latest stage. The uplift processes were not uniform in space, and different plutons had somewhat different uplift processes. There existed commutative uplift reparation in time, i.e., the more rapid uplift and the larger uplift range the pluton at the early stage was, the slower uplift and the smaller uplift range the pluton at the late stage became. Based on thermochronologic analysis and regional tectonic setting as well as other geological data, the authors consider that the lower crust of Wufengxian, Dayishan and Qitianling areas was thickened by 4100~7700m as a result of tectonic stacking in late Middle Triassic, suggesting that there existed violent intracontinental orogeny at the early stage of the Indosinian movement. The Late Yanshanian uplift and the cooling of the plutons were caused by early tectonic denudation and late weathering erosion, which led to the good deposition response in basins. The latest rapid uplift in southeast Hunan was a regional integral uplift.

湘东南地区位于南岭中段北缘。本文应用热年代学方法,测定了湘东南地区5个侵入体的热历史,进而分析湘东南中新生代的隆升过程,并结合区域构造背景,对热演化过程与构造发展过程之间的关系进行了探讨。研究结果表明,湘东南地区中新生代山体隆升过程总体上分为由较快速→快速→缓慢→快速的4个阶段,222~146.Ma期间以0·069mm/a的平均速率较快隆升,146.~94·11Ma期间以0·113~0·186mm/a的平均速率快速隆升,94·11~14·8Ma期间以0·014~0·028mm/a的平均速率缓慢隆升,14·8Ma~0·0Ma以0·143~0·295mm/a的平均速率快速隆升。晚近时期的隆升总体呈加速趋势。隆升过程在空间上具有非均匀性,不同岩体间隆升过程存在差异。地壳隆升过程在时间上具有明显的互补性,早期具较快速或较大幅度隆升的岩体,通常伴随着晚期相对较慢和较小幅度的隆升。根据热年代学分析结果,结合区域构造背景和其它地质资料,推断五峰仙、大义山、骑田岭等地区在中三叠世后期因构造叠置增厚了4100~7700m以上,证明印支运动早期为强烈的陆内挤压造山运动。燕山晚期岩体隆升和降温由早期构造剥蚀和晚期风化剥蚀造成,并具...

湘东南地区位于南岭中段北缘。本文应用热年代学方法,测定了湘东南地区5个侵入体的热历史,进而分析湘东南中新生代的隆升过程,并结合区域构造背景,对热演化过程与构造发展过程之间的关系进行了探讨。研究结果表明,湘东南地区中新生代山体隆升过程总体上分为由较快速→快速→缓慢→快速的4个阶段,222~146.Ma期间以0·069mm/a的平均速率较快隆升,146.~94·11Ma期间以0·113~0·186mm/a的平均速率快速隆升,94·11~14·8Ma期间以0·014~0·028mm/a的平均速率缓慢隆升,14·8Ma~0·0Ma以0·143~0·295mm/a的平均速率快速隆升。晚近时期的隆升总体呈加速趋势。隆升过程在空间上具有非均匀性,不同岩体间隆升过程存在差异。地壳隆升过程在时间上具有明显的互补性,早期具较快速或较大幅度隆升的岩体,通常伴随着晚期相对较慢和较小幅度的隆升。根据热年代学分析结果,结合区域构造背景和其它地质资料,推断五峰仙、大义山、骑田岭等地区在中三叠世后期因构造叠置增厚了4100~7700m以上,证明印支运动早期为强烈的陆内挤压造山运动。燕山晚期岩体隆升和降温由早期构造剥蚀和晚期风化剥蚀造成,并具有良好的盆地沉积响应。湘东南地区晚近时期的快速隆升是区域性整体抬升。

 
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