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tectonic transition     
相关语句
  构造转换
     there is dike rock invasion during tectonic transition,and 4 mineralization periods are classified,among which the early ductile-brittle environment result in the main mineralization belt;
     构造转换过程均有脉岩上侵,依此将主要成矿过程划为4个期次,其中早期的韧脆性环境形成主体矿化带;
短句来源
     The study shows that not only the extended tectonic systems are developed in the tectonic transition sections, also the transition sections are grown in the extended tectonic system, there are different oil control mechanisms in different tectonic systems.
     研究表明,构造转换带不仅可以发育于伸展断裂系统,同时也可以发育于走滑断裂系统,在不同的构造体系中具有不同的控油机制;
短句来源
     It is considered that different tectonic transition sections with different oil control mechanisms are developed in Xuzhuang and Chenbao Areas, by which a theoretical basis is provided for further exploration and development in the area.
     认为许庄、陈堡地区分别发育不同性质的构造转换带,具有不同的控油机制,这一认识为该区的进一步勘探开发提供了理论依据。
短句来源
     The Zhangbaling uplift is located in a tectonic transition zone(collision-amalgamation zone)between the North and South China blocks. It is bounded on the west by the famous Tanlu fault zone, and on its eastern side there occurs a foreland fold-and-thrust belt of the pre-Jurassic sedimentary cover of the Yangtze block.
     张八岭隆起位于华南地块与华北地块碰撞拼接的构造转换部位,其西界为著名的郯庐断裂带,东缘属于扬子地块盖层前陆逆冲褶皱构造带。
短句来源
  “tectonic transition”译为未确定词的双语例句
     This indicates that the tectonic transition happened during 143~113 Ma in the Liaodong Peninsula.
     从而表明在晚侏罗纪-早白垩纪期间(143~113Ma)辽东半岛经历了区域构造体制变革。
短句来源
     Fan HR,Hu FF,Yang JH,Shen K and Zhai MG.2005.Fluid evolution and large-scale gold metallogeny during Mesozoic tectonic transition in the eastern Shandong province.
     胶东中生代构造体制转折过程中流体演化和金的大规模成矿
短句来源
     Linking the common p-T-t path for collisional orogeny to the tectonic evolution of metallogenic provinces in China shows that the large-scale granitic magmatism and metallogenesis in China occurred in a decompression-geothermal increase regime during tectonic transition from collisional compression to extension, instead of post-collisional tectonism.
     通过联系各成矿省地质构造演化与碰撞造山带 p T t轨迹 ,确定各成矿省成矿作用和花岗岩浆作用均爆发于陆陆碰撞过程挤压伸展转变期的减压升温体制 ,而不是碰撞后。
短句来源
     Tectonic transition in the east of China resulted in a distinct difference between Indosinian and Yanshanian tectonic evolutions, and also their stacking and distribution patterns in space and time of basins in the North China plate.
     华北板块东部印支和燕山期构造演化差异、盆地分布格局变迁及其空间叠合关系是中国东部构造变化的结果。
短句来源
     130 Ma,coeval with the tectonic transition from continental-collisional compression to extension. Finally,we interpret the development of the metallogenic magma-fluid systems in NE China using the CMF model at orogen-scale.
     厘定大规模成岩成矿时间为130Ma左右,构造环境是古亚洲洋闭合后陆陆碰撞过程的挤压-伸展转变体制,并以矿集区尺度的CMF模式解释了浅成低温热液矿床岩浆-流体系统的发育机制。
短句来源
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  相似匹配句对
     Transition of Tectonic and Dynamic Regime and Mineralization
     构造动力体制转换与成矿作用
短句来源
     ⑥ time and space of transition of tectonic systems,;
     ⑥构造体制转折期与转折部位;
短句来源
     Employment in Transition
     变革中的劳动就业
短句来源
     and transition phase.
     转变 ,并析出过渡相。
短句来源
     Tectonic in Architecture
     论建筑中的结构造型
短句来源
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  tectonic transition
The mid-Cretaceous granitoids of the Hohonu Batholith were generated during a period of rapid tectonic transition from crustal thickening during collision to crustal thinning and core complex formation during extension.
      
It is concluded that the Cu-Pb-Zn mineralizations in the Dajing and Caijiaying deposits resulted from the identical tectono-thermal event of magma-fluids induced by Mesozoic tectonic transition and extension in the eastern part of North China Craton.
      


This paper describes an understanding on the correlation of various blocks in the fault-folded belt in the northern part of western border of Shanxi- Gansu-Ningxia basin and the location of its eastern border which is different from the majority of opinions so far published.It is suggested that various types such as vertical shearing,high angle shrust,compressional pairs and low angle overthrust are formed due to the non-synchronization of the disp- lacement resulting from the background environment and boundary...

This paper describes an understanding on the correlation of various blocks in the fault-folded belt in the northern part of western border of Shanxi- Gansu-Ningxia basin and the location of its eastern border which is different from the majority of opinions so far published.It is suggested that various types such as vertical shearing,high angle shrust,compressional pairs and low angle overthrust are formed due to the non-synchronization of the disp- lacement resulting from the background environment and boundary conditi- ons.This paper points out that the western dipping of the fault plane in Majiatan Area (as usually accepted) refers really to the fault system ot the overthrust sheet and is in a different type with the fault system with east dipping fault plane characterizing the feature of the overthrust sheet front zone,so that they cannot be correlated.The fault plane of the compressio- nal zone of the overthrust sheet front in Majiatan Area dips to the east also,and is in consistent with the same zone in Hengshanbao and Tiekesu- miao Areas.An assumption on the variation of the type of the sheet front is suggested that various blocks in this region are different expressions for- med under the same geostress field,and thus it is not necessary to give an explanation as to whether it is compressive torsional or tensile in nature regarding to different sections.It is also suggested that the east border of this region cannot be recognized according to fault systems or the syncline axis.A concept of tectonic transition is suggested in this paper in this res- pect.This paper suggests also that the tectonic of Tiekesumiao sag should be rediscussed.

本文对西缘断褶带(北段)的区块对比及其东界位置提出了新的观点。认为在若干千米长的推覆带上,因背景环境、边界条件造成的位移不同步,可以形成纵向剪切、高角度掩冲、挤压对峙和低角度推覆等多种类型。指出所谓马家滩地区断面西倾实指各种冲断席的断层系,与表征前缘推挤带特征的断面东倾断层系统不属同类,不能对比。马家滩地区前缘推挤带断层断面同样是东倾的,和该带的横山堡地区,铁克苏庙地区一致。从而提出了推覆体前缘带形式变化说,认为各区块是同一地应力场下的不同表现形式,无须做分段的扭压拉张等解释。同时不同意以断层或向斜轴划分该区东界,提出了构造过渡的观点,并建议重新考虑铁克苏庙坳陷的大地构造单元属性。

There are level planation surfaces,terraces and unsymmetrical landforms in the Huangshui River drainage area,west to Lanzhou The unsymmetrical landform can be divided into the simple unsymmetrical gully,the step unsymmetrical gully and unsymmetrical range,which were formed by the erosion of the surface water during the unsymmetrical rising of the earth's surface This kind of landform shows an important tectonic transition at 0.15 MaB P .Moreover,it indicates that the uplift of the Qinghai Tibet Plateau...

There are level planation surfaces,terraces and unsymmetrical landforms in the Huangshui River drainage area,west to Lanzhou The unsymmetrical landform can be divided into the simple unsymmetrical gully,the step unsymmetrical gully and unsymmetrical range,which were formed by the erosion of the surface water during the unsymmetrical rising of the earth's surface This kind of landform shows an important tectonic transition at 0.15 MaB P .Moreover,it indicates that the uplift of the Qinghai Tibet Plateau is even in the long time interval (0.2—0 9 Ma),while it is unevenly in the shorter time interval (0.01—0 1 Ma) By the action of its own gravity after the Plateau rose to the height of 3 0—3 7 km,and the stress came from the Indian Plate,the Qilian Mountains were uplifted largely at 0 15 MaB P ,and the harsh environment in the northwest China began at the same time

在湟水河流域发育夷平面、阶地和不对称的山脉、沟谷等地貌,对阶地、夷平面上的条带状水成黄土层的倾向和倾斜率的系统测量,反映出流域内地表的抬升。根据对称性可分为4 个阶段,隆升在大的时间尺度上是均匀的,在小尺度上是不均匀的;当高原隆升到一定高度后,受印度板块侧向挤压,高原向四周的应力的共同作用使祁连山隆升,并伴随着气候恶化。

The seismic and stratigraphic data on the Jizhong basin have been analysed to determine the tectonic deformation and evolution during the Mesozoic.Early stage (Triassic) of evolution of the basin is marked by WNW-striking compressive structures,where mainly preserved,named Xushui-Renqiu ridge and Liuxi-Dawangzhuang ridge during Indosinian movement. The following stages (from Jurassic to Cretaceous) are marked by NE-NNE-striking compressive structures and NW-striking extended structures during Yanshan movement.More...

The seismic and stratigraphic data on the Jizhong basin have been analysed to determine the tectonic deformation and evolution during the Mesozoic.Early stage (Triassic) of evolution of the basin is marked by WNW-striking compressive structures,where mainly preserved,named Xushui-Renqiu ridge and Liuxi-Dawangzhuang ridge during Indosinian movement. The following stages (from Jurassic to Cretaceous) are marked by NE-NNE-striking compressive structures and NW-striking extended structures during Yanshan movement.More of the NE-NNE-striking compressive structures are faults except Gaoyang-Wuji ridge.The faults mainly included East Taihang mountain normal fault in the west and Maxi thrust,Litan thrust,Ningjing thrust and Xinhe thrust in the east.The latter composed of nappe system during Yanshan movement.The transitional period is between the middle Jurassic and the early Cretaceous and represents a tectonic transition from proto-Asia tectonic tract (PATT) to circum-Pacific tectonic tract (RPTT).Therefore,the promising traps during the Mesozoic for hydrocarbon exploration are buried hills and drape anticline traps associated with NW-striking extended structures.

冀中坳陷中生代构造变形主要包括印支期古亚洲域的北西西向和燕山期环太平洋域的北东、北北东向压性构造及其配套的北西向张性构造。前者主要是残存的徐水─任丘古隆起带,次要则如留西─大王庄古隆起带等;后者除了北东向的高阳─无极隆起带以外,则以同向的断裂构造为主。西界为太行山东伸展断层,而东界为 (古 )马西逆冲断层和 (古 )里坦逆冲断层以及 (古 )宁晋逆冲断层、 (古 )新河逆冲断层等构成叠瓦状逆冲系统。古亚洲域向环太平洋域的转换时期在中侏罗─早白垩世之间。中生代构造研究可以为冀中坳陷深层油气提供潜山圈闭、下第三系披覆背斜圈闭和岩性圈闭等有利勘探目标。

 
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