大地构造的

基本解释 (translations)

geotectonic

与大地构造的相关的网络例句 [注：此内容来源于网络，仅供参考]

HUANG Jiqing gave a brilliant exposition with E. Argand's mobilism thought as to the dynamical evolution process of the tectonics in On Major Tectonic Forms of China.

在《中国主要地质构造单位》中，他运用阿尔冈活动论的思想，阐述了中国大地构造的动力演化过程。

1:250000 geological mapping has further revealed the mysteries of the tectonics of the Qinghai-Tibet Plateau. The Altun Mountains are not of the Tarim massif, but a part of the Kunlun-Qilian-Qinling orogenic system; the Altun fault is a large transform fault; the Muztag-Maqên suture zone and Jinshajiang suture zone are both Variscan ones; the Songpan-Garzê area in the Triassic was a huge turbidite basin on the southern margin of Laurasia; the Gangdise belt underwent the important Indosinian orogenic movement; an ocean basin that persisted from the Paleozoic to Triassic did not exist, i.e. the so-called Paleo-Tethys or permanent Tethys was not in existence in the Qinghai-Tibet Plateau. In the Paleozoic, most parts of China, including the Sino-Korean, Yangtze and Tarim massifs and the Qinghai-Tibet Plateau, were located in south of the main ocean basin—the Central Asian-Mongolian sea way—of the Paleo-Asia ocean, belonging to the northern margin of Gondwana. The Yarlung Zangbo and Bangong -Nujiang belts were twins in the Tethyan Ocean, which began to develop into two ocean rift belts in the Triassic. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be subducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian, Yanshanian and Himalayan stages.

1：25万地质填图进一步揭开了青藏高原地区大地构造的奥秘：阿尔金山是昆仑，祁连-秦岭造山系的一部分；阿尔金断裂确是一条大型转换断层；木孜塔格-玛沁缝合带和金沙江缝合带均是华力西缝合带；松潘甘孜三叠系沉积盆地是劳亚大陆南部边缘的浊积岩盆地；冈底斯带曾经历了重要的印支造山运动；不存在从古生代延续到三叠纪的大洋盆地，即不存在所谓古特提斯或永久特提斯；古生代时期，在青藏高原地区亦不存在具古生物，古地理分隔意义的大洋盆地，当时，包括中朝，扬子，塔里木以及青藏高原地区在内的中国大部分均位于古亚洲洋主洋盆——中亚-蒙古带之南，属冈瓦纳大陆结构复杂的北部边缘；雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹，它们均是从三叠纪起就发展成大洋裂谷带的；以雅鲁藏布江带为主洋盆带的特提斯洋，从三叠纪晚期开始消减，经历了印支，燕山，喜马拉雅3个阶段脉动式板块汇聚造山过程。

Taihangshan as a symmetric axis and Shanxi belt, located in the relatively uplifted portion of upper mantle in regard to their depths. Therefore, it is...

因此，作者认为，重力和重力均衡调整的作用在很大程度上影响了华北大地构造的发育，塑造了其地壳结构的基本形态，因而也就制约了华北地区的地震活动。

Taihangshan as a symmetric axis and Shanxi belt, located in the relatively uplifted portion of upper mantle in regard to their depths. Therefore, it is consi...

因此，作者认为，重力和重力均衡调整的作用在很大程度上影响了华北大地构造的发育，塑造了其地壳结构的基本形态，因而也就制约了华北地区的地震活动。

There's 132 under the United States, an average of 5.36 to 7.24 cubic miles in size at an average of 1.5 to 4.5 miles underground, built, by and large, most of them in areas away from geotectonic areas - but there's going to be lots of new geotectonic faults established when you have force 11, 12, 13, 14 earthquakes hit the Earth.

在美国地下有132个这样的基地被修建，尺寸大小上平均有5.36至7.24立方英里，平均深度为1.5到4.5英里（2.4~7.2千米），大体上，他们中的大多数在远离大地构造的区域——但会有很多新的构造断层形成，当你有强有力的11、12、13、14级地震来袭地球。

In view of an analysis from lithospheric geoid, horizontal stress and existing seismic tomographic data and so on, they show that Chinese mainland and adjacent area is controlled by mantle dynamics of interaction, mutual influence and constraint by western Pacific ocean plate, Indian plate and circum-Siberian arc tectonics that formed after Paleo-Asian ocean closed, which consist of three tectonic areas, with on the base of the Tethyan tectonic realm. Overall tectonic framework of the Chinese mainland is outwards obduction along main tectonic borders within shallow crust and inwards subduction and convergence within deep lithospheric mantle from south-western, south-eastern and northern parts, respectively.

基于岩石圈大地水准面异常、水平应力场和地震层析等地球物理资料综合分析可知，中国大陆及其毗邻地区在特提斯构造基础上，处于西太平洋板块、印度板块和古亚洲洋及其闭合之后环西伯利亚弧形等三大全球构造体系域相互作用、相互影响和相互制约的地幔动力学控制之下，总体大地构造格局是浅部地壳分别沿主要构造边界向外仰冲，深部岩石圈地幔则从西南、东南和北部向中国大陆俯冲会聚，使之整体处于地幔会聚挤压的大地构造背景。

From the tectonic structure point of view, the collision of the two plates forms a series of orogenic belt, while in the frontal edge of the subducting plate , it is always shaped into the foreland basin.

从大地构造的观点看，两个板块相互碰撞形成挤压造山带，常常在俯冲板块的前缘形成前陆盆地。

This paper collects the latest data in different fields of geological researches on mid-Asian area such as regional geology, Bouguer gravity, aeromagnetic, satellite magnetic, DEM, seismic tomography, modern earthquake, isotope age, deposit occurrence. In this paper, GIS, gravity and magnetic data processing software, and advanced image processing software are employed for the first time to analyze and process large amount of complex data, from which much helpful information were obtained. Such information offered reliable basic data for doing assessment and interpretation, therefore make possible to put forward, from geophysical point of view, a set of new views and methods in studying of tectonic of mid-Asian area.

本文收集了中亚地区区域地质、布格重力、航磁、卫星磁力、地震层析成像、现代地貌、现代地震、同位素、已有矿床分布等多源地学信息的最新成果，首次利用地理信息系统、重磁数据处理软件、先进的图像处理软件对中亚地区的多源数字化数据进行集成，透过纷繁复杂的现象，总结规律，从中提取了许多有用的信息，为判识和综合解译提供了可靠的基础资料，从地球物理角度提出了一套研究中亚地区大地构造的新思路、新方法。

The geology and mineral resources department′s new round investigating work in geological mapping,i.e.1∶200 000 geological mapping at nonsmith stratigraphy of multicycle mountain building belt takes activity theory and continent investigating dynamic geology as its guiding ideology,and is to show orogenic belts′ structure formation evolution and its tectonics framework fundamental characteristics,especially its orogenic process and today′s orogenic belt′s three-dimensional structure.

作为原地矿部新一轮地质填图调查工作，即在多旋回造山带非史密斯地层区进行1∶20万填图，以活动论和探索大陆动力学为指导思想，旨在着重表现造山带的结构、形成、演化及其大地构造的基本特点，尤其侧重于其造山过程和现今造山带的三维结构。

According to study the tectonic facies map of Balkhash- Junggar region, the article establishment geology conceptual model from two aspects which are tectonic setting and tectonic evolution. Based on the idea of information science, the article using Geodatabase data model and discussing feature class, attribute table and their mutual relations to construct tectonic facies spatial data model of Balkhash - Junggar region that based on the idea of information science.

闭于巴人喀什-准噶人地域大地构造相图入行剖析，自卑地构造空间序列和大地构造时光序列两个角度来树立地量概念模型，基于信做科教的念惟，当用Geodatabase数据模型，谈论大地构造相图的要荤类、属性外及其之间的互相闭解，构建基于信做科教念惟的巴人喀什-准噶人地域大地构造相图空间数据模型。

与大地构造的相关的网络解释 [注：此内容来源于网络，仅供参考]

architectonic：地质构造的

architectonic geology 构造地质学 | architectonic 地质构造的 | architectonics 大地构造学

geotectonic subsidence：大地构造下陷

join the flats 使成为连贯的一体 | geotectonic subsidence 大地构造下陷 | colour multiplexing 彩色信号多路传输系统, 彩色副载频正交调制

tectonic：大地构造的

syngas production from NG 天然气造气 | tectonic 大地构造的 | transformation reation 变换反应

tectonic map：大地构造图

化油器的作用是:根据发动机在不同情况下的需要,将汽油气化,并与空气按一定比例大地构造图 大地构造图(tectonic map)是表示一个大区域乃至一个或几个大陆、大洋主要构造特征的地质图件,如亚洲大地构造图.

geotectonic：大地构造的

geotectonic valley 大地构造谷 | geotectonic 大地构造的 | geotectonics 大地构造

geotectonic cycle：大地构造旋回

释文:又称造山旋回(orogenic cycle)、褶皱旋回(folding cycle)、大地构造旋回(geotectonic cycle)等. 法国地质学家贝特朗(M Bertrand,1886~1887)用分析角度不整合的方法确立了地槽区内的褶皱运动具有周期性. 通过对西欧和北美各个褶皱区进行比较,

geotectonic valley：大地构造谷

geotectonic unit 大地构造单位 | geotectonic valley 大地构造谷 | geotectonic 大地构造的

geotectonics：大地构造

geotectonic 大地构造的 | geotectonics 大地构造 | geotector 地震检波器

geotectonics：大地构造学/构造地质学

geotectonic /大地构造的/ | geotectonics /大地构造学/构造地质学/ | geotector /地音探测器/

seismotectonic map：地震大地构造图

seismotectonic line 地震构造线 | seismotectonic map 地震大地构造图 | seismotectonic 地震构造的