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tectonic map
相关语句
  构造图
     THEORY AND METHOD OF CARTOGRAPHY OF PLATE TECTONIC MAP
     板块构造图的制图理论与方法探讨
短句来源
     On the basis of the obtained results and referenced data from colleagues in Vietnam and abroad, the faulting tectonic map of SE Asia at 1: 4 000 000 scale and of Vietnam and adjacent areas at 1: 1 000 000 scale have been compiled.
     在所得结果 的基础上参考了越南国内外同行的一些资料编制了东南亚、越南及邻区的断裂构造图,其比例尺分别为1∶4百万 和1∶1百万。
短句来源
     Based on the analysis of the forms and the comparability in configuration of fault and fracture, the information dimension of faults on tectonic map T5, T2 and that of fracture in ten cores from research formation J3b were calculated, then the factors affecting their information dimension were analyzed, finally, the distribution of fracture in the research region is predicted.
     在详细剖析断裂和裂缝组成和结构相似性的基础上,计算了贝尔断陷T5和T2两层构造图上断裂信息维和10口井布达特群岩心裂缝信息维,分析了影响断裂和裂缝信息维的因素,达到了从断裂信息维去预测裂缝分布的目的.
短句来源
     The tectonic map of the major active faults of China and its environs in the Cenozoic, compiled recently by the present author, shows that the influence of the Indian plate collision on the evolution of tectonic structures of China is far more intensive than that of the Mesozoic Pacific-Asian plate convergence since the Jurassic.
     由作者新编的中国主要活动断裂构造图显示 ,印度板块的碰撞对中国地质构造演化的影响远比自中生代侏罗纪以来太平洋亚洲板块会聚造成的影响更为强烈。
短句来源
     Based on the establishment of the plate tectonic map of Qinghai-Xizangplateau (1: 1000000) and the plate tectonic and geological map of the north margin ofQaidum Basin (1: 500000), in consideration of the scholar's suggestions on the two maps,the author has mainly discussed the theory and method of cartography of regional platetectonic map.
     通过编制区域性1:300万“青藏高原板块构造图”和1:50万“柴达木北缘板块构造地质图”的体会,并结合国内学者对这两份图件的审查意见及建议,重点讨论有关区域性板块构造图编制的理论与方法,供区域地质工作者参考。
短句来源
更多       
  大地构造图
     TECTONICS AND EVOLUTION OF THE EASTERN TIANSHAN MOUNTAINS-A BRIEF INTRODUCTION TO “TECTONIC MAP (1 : 500 000) OF THE EASTERN TIANSHAN MOUNTAINS OF XINJIANG
     东天山大地构造及演化——1:50万东天山大地构造图简要说明
短句来源
     The 1:2,000,000 Tectonic Map of Xinjiang and its explanatory notes were completed in 1987 under the guidance of the theory of polycyclic geosyncline and platform advanced by Prof. Huang Jiqing. On the basis of a systematic summarization and study of the data obtained through more than 30 years of regional surveys and scientific researches and other relevant data, the tectonic units and cycles have been distinguished and discussed.
     1987年完成的新疆1∶200万大地构造图及说明书,以黄汲清教授倡导的多旋回槽台学说为指导,在系统总结研究了30年来区调、科研及其它有关资料基础上,对构造单元、构造旋回进行了划分和论述。
短句来源
     "Deep structure map or Asia" is ohe of basic figures relating to "Tectonic map of Asia continent and sea".
     “亚洲深部构造图”是《亚州陆海大地构造图》的基础图件之一.
短句来源
     In the Tectonic Map of Asia Wulinsynan is situated in the southern segment of the East Asia crustobody, at the northeastern end of the West Hunan—East Guizhou geodome series of thc Yunnan—Guizhou diwa region.
     在亚洲大地构造图中,武陵源位于东亚壳体南段,云贵地洼区的湘西黔东地穹列的东北端。
短句来源
     In the 1970s, under his direction, his students combined plate tectonics with theory of polycyclic movements, the plate suture zones were first particularly plotted on the Tectonic Map of China, and the three tectonic types of Asia which were advanced by HUANG Jiqing in 1945 developed into three tectonic domains—the paleo-Asian domain, the circum-Pacific domain and the Tethyan domain from the viewpoint of global dynamics.
     2 0世纪 70年代 ,他指导他的学生将多旋回思想与板块构造结合 ,在中国大地构造图上首次详细标绘了中国境内的板块缝合带 ,从全球动力学角度 ,将他 1 94 5年提出的亚洲三种构造型式发展为古亚洲、特提斯和滨太平洋三大构造域。
短句来源
  “tectonic map”译为未确定词的双语例句
     SUGGESTIONS IN COMPILING A TECTONIC MAP
     构造地质图中若干问题的浅析
短句来源
     By classifying tectonic sequence, confirming corresponding prototype basin, analyzing paleo-tectonic stress fields in different periods, plotting correlative tectonic map based on 297 explore wells, and analyzing the traits of the remaining depressions producing hydrocarbon and their migration rules in the Ordovician, the author studied the basement of the basin;
     鄂尔多斯盆地及其周缘地区沉积盖层可划分为五大构造层序,盆地的形成和演化分为六大构造阶段:太古代至古元古代基底形成阶段、中新元古代克拉通内裂陷槽或坳拉槽演化阶段、震旦纪—早古生代华北陆表海盆演化阶段、晚古生代—早中生代华北克拉通坳陷演化阶段、中生代中晚期大鄂尔多斯内陆盆地演化阶段及独立鄂尔多斯盆地的形成、新生代周缘断陷盆地演化阶段。
短句来源
     In China geological and tectonic map, this region is referred to as the North China and some south area of it.
     这个区域是我国地震活动强烈的地区之一,曾多次发生强烈破坏性地震,区内既有大陆内部的碰撞造山带(秦岭-大别造山带),又有贯通本区南北的大型断裂带(郯庐断裂带)和大型重力梯级带(太行山),地质构造十分复杂。
短句来源
     After regional tectonic map complition and detail observation at key sections, the Longquanguan Sanggan tectonic belt(LSB)trending in NNE direction is recoginzed in the central part of North China Craton and is characterized by large scale ductile shear zones, granitic belt and numerous high pressure granulite lenses or slices.
     通过区域构造编图及重点地段的详细研究,在华北克拉通中北部识别出一条NNE向的构造带——龙泉关-桑干带,它以大规模的韧性剪切带网络、重熔钾质花岗岩带、数量众多的高压麻粒岩构造透镜体或岩片为特征。
短句来源
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  tectonic map
Kurz on "Tectonic map and overall architecture of the Alpine orogen"
      
Tectonic map and overall architecture of the Alpine orogen Comment on an article by Stefan M.
      
The new tectonic map of the Alps is based on the combination of purely structural data with criteria regarding paleogeographical affiliation and/or tectono-metamorphic evolution.
      
Tectonic map and overall architecture of the Alpine orogen
      
Thirteen seismic zones are defined on a regional seismic and tectonic map presented for the area.
      
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By carefully interpreting the Xizang Landsat imageries, we have discovered a series of active faulting belts and recent basins. Moreover, magmatism and volcanic and geo thermal activities may come very intensive in Xizang. We have applied the Landsat image to making the seismo-tectonic map of Xizang. It shows that the Xizang plateau has three main structural types. The south Xizang area consists of many closely parallel and rectilinear lineaments which indicate an intensively compressive deformation; the...

By carefully interpreting the Xizang Landsat imageries, we have discovered a series of active faulting belts and recent basins. Moreover, magmatism and volcanic and geo thermal activities may come very intensive in Xizang. We have applied the Landsat image to making the seismo-tectonic map of Xizang. It shows that the Xizang plateau has three main structural types. The south Xizang area consists of many closely parallel and rectilinear lineaments which indicate an intensively compressive deformation; the middle Xizang area presents continually lenticular-like structures which show a plastic deformation; and the Qiangtang plateau possesses conjugated fracture deformation. These properties determine the seismic activities in the Xizang region and the three seismic areas can be classified.There have been more than 284 earthquakes with magnitude above 5 since 1870. We have subdivided the seismic events occuring during 20 th century into three periods, each extending about 30 years. Now the third period is going to come to an end.Finally we point out that earthquake frequency and intensity in Xizang are related to the collision of the India-Eurasia plate.

陆地卫星影象表明西藏地区存在一系列活动断裂带,晚第三纪以来的新生盆地和火山活动都十分强烈。从卫星照片中的线性构造及其组合特征分析,西藏高原具有三种不同的构造组合,雅鲁藏布江以南多为近东西向线性构造,为强烈挤压的形变特征,中部多为连续分布的透镜状构造,反映了地壳物质塑性流动的形变特征,羌塘高原则为共轭破裂的形变特征。这些特征客观地反映了西藏高原各块体之间的力学性质和介质条件的差异,也控制了西藏地区的地震活动性。

This paper has briefly sum(?)larized the experiences in using the diwa theory in compiling the tectonic map of Anhui Province (1:500000)and in studying the geotectonics and metallogeny in Anhui Province. Some new arguments on several important geological problems in the region are proposed, such as the existence or absence of some deep-seated fault zones, thc geotectonic nature of the Middle-Lower Changjiang (Yangtze) region and the tectonic designation of the Dabieshan Mountain region, etc.) Some...

This paper has briefly sum(?)larized the experiences in using the diwa theory in compiling the tectonic map of Anhui Province (1:500000)and in studying the geotectonics and metallogeny in Anhui Province. Some new arguments on several important geological problems in the region are proposed, such as the existence or absence of some deep-seated fault zones, thc geotectonic nature of the Middle-Lower Changjiang (Yangtze) region and the tectonic designation of the Dabieshan Mountain region, etc.) Some new complementary ideas are suggested in several aspects such as the structural features, tectonic movement styles and metallogenic models.

本文简介绍了,以地洼学说为指导编制《1/50万安徽省大地构造图》和开展《安徽省大地构造与成矿》研究的体会,以及对该区一些重大地质问题,如深断裂是否存在?长江中、下游大地构造的性质,大别山区的构造归属等取得的新认识。并在构造型相、运动型式、成矿演化模式方面,提出了新的补充意见。

In this paper,the three-dimensional velocity images beneath the Chinese continent and adjacent regions are reconstructed using P-wave travel time residuals of regional and distant earthquakes recorded by the Chinese seismic networks and ISC.The main results are as follows:1.The velocity images display clearly the lateral heterogeneity of the crust and upper mantle beneath the Chinese continent and adjacent regions, which persists down to at least 1100 km deep.The correlation between the velocity image of the...

In this paper,the three-dimensional velocity images beneath the Chinese continent and adjacent regions are reconstructed using P-wave travel time residuals of regional and distant earthquakes recorded by the Chinese seismic networks and ISC.The main results are as follows:1.The velocity images display clearly the lateral heterogeneity of the crust and upper mantle beneath the Chinese continent and adjacent regions, which persists down to at least 1100 km deep.The correlation between the velocity image of the upper mantle and the known surface geological feature can be traced down to a depth of 110km.Below 220 km this correlation is hardly seen.2.The velocity images at depths of 45-0km and 45+0km show clearly that the crust of the Chinese continent is divided into two parts approximately by the 102.5°E longitude.3.The velocity image at a depth of 110 km shows that velocity anomalies appear in block patterns.Comparing the image to the tectonic map of China,we find that the Yangtze para-platform and the Tarim platform correspond to high velocity zones,the Sino-Korean paraplat-form appears mostly as a low velocity anomaly,the South China fold system is a low velocity zone.Note that a dumbbell-shaped east-west trending high-velocity zone exists along the Himalayas at the southern margin of the Tibetan block.4.The velocity image at a depth of 220 km shows that low-velocity zones of the asthenos-phere exist under many areas in the Chine.se continent.Similar to the velocity images of 45-0km and 45+0km,the images of 400 km and 600 km also indicate that a strip of about 200 km wide near 102.5°E divides the Chinese continent into two tectonically different parts.This means that the tectonic differences between the eastern and western part of the-Chinese contnent may exist in the whole upper mantle.

本文利用中国地震台网及ISC提供的区域地震和远震的P波走时数据,重建了中国大陆及其邻近地区的三维速度图象。 主要结果是:1.本文给出的速度图象揭示了中国大陆及其邻近地区的地壳和上地幔速度存在明显的横向不均匀性,这种不均匀性甚至在下地幔的1100km深度还依然存在。上地幔的速度图象同地表已知的地质构造特征的相关性可以追踪到110km,从220km以下很难找到它们之间的明显关系。2.45~(-0)km和45~(+0)km深度处的速度图象明显地表示出中国大陆的地壳厚度可以102.5°E附近为界分为两部分:其东部地壳薄,厚度都小于45km;西部有一条自若尔盖—松潘(34°N,102.5°E附近)向西北沿38°N往西至塔里木盆地南缘的分界线;其南部除滇西南之外,整个青藏高原的地壳厚度都大于45km;其北部除天山山脉之外,地壳厚度一般不大于45km.3.110km深度处的速度图象表明,速度异常呈块状分布。同中国大地构造分区略图比较之后发现,其中,扬子准地台和塔里木地台对应于高速区,中朝准地台则大都表现为低速异常;华南褶皱系为低速区,青藏地块南缘喜马拉雅和冈底斯念青唐古拉褶皱系则表现为高速异常。4.220km深度处的速度图...

本文利用中国地震台网及ISC提供的区域地震和远震的P波走时数据,重建了中国大陆及其邻近地区的三维速度图象。 主要结果是:1.本文给出的速度图象揭示了中国大陆及其邻近地区的地壳和上地幔速度存在明显的横向不均匀性,这种不均匀性甚至在下地幔的1100km深度还依然存在。上地幔的速度图象同地表已知的地质构造特征的相关性可以追踪到110km,从220km以下很难找到它们之间的明显关系。2.45~(-0)km和45~(+0)km深度处的速度图象明显地表示出中国大陆的地壳厚度可以102.5°E附近为界分为两部分:其东部地壳薄,厚度都小于45km;西部有一条自若尔盖—松潘(34°N,102.5°E附近)向西北沿38°N往西至塔里木盆地南缘的分界线;其南部除滇西南之外,整个青藏高原的地壳厚度都大于45km;其北部除天山山脉之外,地壳厚度一般不大于45km.3.110km深度处的速度图象表明,速度异常呈块状分布。同中国大地构造分区略图比较之后发现,其中,扬子准地台和塔里木地台对应于高速区,中朝准地台则大都表现为低速异常;华南褶皱系为低速区,青藏地块南缘喜马拉雅和冈底斯念青唐古拉褶皱系则表现为高速异常。4.220km深度处的速度图象表明,中国大陆相当多的地区软流层有明显的显示。5.同45~(_0)km和45~(+0)km的速度图象一样,400km和600km的速度图?

 
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