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tectonic syntaxis
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  “tectonic syntaxis”译为未确定词的双语例句
     REMARKABLE PROGRESSES IN STUDY ON DEFORMATION AND KINEMATICS OF THE EASTREN HIMALAYAN TECTONIC SYNTAXIS
     东喜马拉雅构造结变形与运动学研究取得重要进展
短句来源
     Garnet pyroxenite in the Namjagbarwa Group-complex in the eastern Himalayan tectonic syntaxis,Tibet,China:Evidence for subduction of the Indian continent beneath the Eurasian plate at 80-100 km depth
     东喜马拉雅构造结南迦巴瓦岩群中的石榴辉石岩——印度大陆向欧亚板块之下俯冲至80~100km深度的证据
短句来源
     Garnet pyroxenite occurs as lenses in granulite-facies metamorphic granitic gneiss and pelitic schist in the Namjagbarwa Group-complex of the eastern Himalayan tectonic syntaxis.
     在东喜马拉雅构造结南迦巴瓦岩群中,石榴辉石岩呈透镜状产于麻粒岩相变质的长英质片麻岩和泥质片岩之中。
短句来源
  相似匹配句对
     Criticize and Tectonic
     批判与建构
短句来源
     Tectonic in Architecture
     论建筑中的结构造型
短句来源
     REMARKABLE PROGRESSES IN STUDY ON DEFORMATION AND KINEMATICS OF THE EASTREN HIMALAYAN TECTONIC SYNTAXIS
     东喜马拉雅构造结变形与运动学研究取得重要进展
短句来源
     The Namjagbarwa syntaxis consists of three tectonic units: the central Himalayan tectonic unit, and marginal Gangdise and Yarlung Zangbo tectonic units.
     南迦巴瓦构造结由其核部的喜马拉雅构造单元和周边的冈底斯构造单元、雅鲁藏布构造单元组成。
短句来源
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Owing to the fact that the later structures had intermittently made use of and reformed the earlier ones, the characteristics of both the succession and the pulsation of the tectonic movement were manifested, by the time the structural features were provided with deformation traces of polyphased tectonic activities, and the mechanical properties of the structural elements were induced to transform for many times. The F, dealt with in this paper is such a faulted structure that represents the polyphased tectonic...

Owing to the fact that the later structures had intermittently made use of and reformed the earlier ones, the characteristics of both the succession and the pulsation of the tectonic movement were manifested, by the time the structural features were provided with deformation traces of polyphased tectonic activities, and the mechanical properties of the structural elements were induced to transform for many times. The F, dealt with in this paper is such a faulted structure that represents the polyphased tectonic syntaxis, and in every period of its generation and evolution its mechanical properties were different each other, thus it was taken as the different structural component of each tectonic system. However it mainly appeared as compresso-shearing property, especially in the course of copper ore-forming stage. The behaviour of this faultedrupture provided the favourable geological environment,in which the copper-bearing ore fluids could move and the metallic elements might concentrate, and so which controlled the emplacement of the lenticular or bedded-like ore bodies.

构造活动的继承性和脉动性特点表现在晚期构造对早期构造的间歇式利用和改造,致使构造形迹具有多期次活动的迹象,结构面的力学性质发生多次转化。本文所论述的F_1断层就是这种代表了多次构造复合的断裂构造,它在发生发展的各个阶段,其力学性质均有差异,成为不同体系的不同成份,但主要呈现出压扭性特征,尤其是在成矿阶段。断裂的这种性质提供了铜矿液运移富集的地质环境,控制了扁透镜状或似层状矿体的产出。

The study of structure and geochemistry in Jinya ore field indicated that the distribution, migration, and accumulation of the ore-forming elements were mainly controlled by tectonization and structural features. The distribution of the anomalous area of the elements was controlled by faults and fractures. All deposits in the ore field are iocated in the intersection of tectonic syntaxis, where the values of the structural confining pressure, the maximum shear stress, and the strain energy are lower. The...

The study of structure and geochemistry in Jinya ore field indicated that the distribution, migration, and accumulation of the ore-forming elements were mainly controlled by tectonization and structural features. The distribution of the anomalous area of the elements was controlled by faults and fractures. All deposits in the ore field are iocated in the intersection of tectonic syntaxis, where the values of the structural confining pressure, the maximum shear stress, and the strain energy are lower. The formation and distribution of the deposits are strictly controlledby NW direction structural system.

对金牙金矿田构造地质及地球化学的研究表明,金牙金矿田成矿元素的分布、迁移和富集是受构造运动及构造形迹控制的。巴合背斜总体上控制了成矿元素的分布;而断裂构造则控制了成矿元素异常的分布。矿床(点)毫无例外地分布于断裂构造复合部位的构造围压、最大剪应力和应变能的低值区,严格受北西向构造(体系)控制。

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. The shear zones are dominated by thrusting in NW-SW direction,resulted in imbrication of basement complex with supracrustal sequences including khondalite series,and isothermal...

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. The shear zones are dominated by thrusting in NW-SW direction,resulted in imbrication of basement complex with supracrustal sequences including khondalite series,and isothermal decompression and uplift of high pressure granulites.Regionally,LSB joints Ordos craton with Fuping Zanhuang craton, which are chiefly composed of Archean TTG granitic rocks khondalites and TTG granitic rocks supracrutal sequences respectively, recorded late Archean tectonic syntaxis process.

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。剪切带以低角度逆冲为主,矿物拉伸线理指示运动方向为NW-SE向。这些剪切带造成东西两侧基底杂岩与表壳岩系包括孔兹岩系的广泛构造叠置,以及高压麻粒岩的近等温减压上隆。从更大的范围看,龙泉关-桑干带处于鄂尔多斯克拉通和阜平-赞皇克拉通之间,并且被五台-吕梁裂谷型绿岩带截切或不整合覆盖。该带应形成于晚太古代,记录了上述两个克拉通斜向拼合的构造过程

 
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