1) orogenic belt
造山带
1.
Rock finite strain and estimation of deformed components of structural blocks in an orogenic belt;
岩石有限应变与造山带构造块体变形要素的估算
2.
Progress in the study of the Early Paleozoic Kunlun orogenic belt;
昆仑早古生代造山带研究进展
3.
Tectonic facies along the Nujiang-Lancangjiang-Jinshajiang orogenic belt in southwestern China;
西南“三江”造山带大地构造相
2) orogen
['ɔ:rədʒin]
造山带
1.
Metallogeneses in the collisional orogen of the Qinghai-Tibet Plateau: Tectonic setting, tempo-spatial distribution and ore deposit types;
青藏高原碰撞造山带成矿作用:构造背景、时空分布和主要类型
2.
Nature of Main Tectono-Lithostratigraphic Units of the Qinling Orogen: Implications for the Tectonic Evolution;
秦岭造山带主要构造岩石地层单元的构造性质及其大地构造意义
3.
Dabieshan Mountain orogen consisted of the south-east Qinling fold Zone,controls the magmatic rock together in southern Henan Province with Guishan-Meishan fault zone and north-east fault.
大别山造山带,是秦岭褶皱带南东的组成部分,它与龟(山)—梅(山)断裂带、北东向断裂共同控制着豫南岩浆岩的分布。
3) orogenic zone
造山带
1.
The characteristics of mineralization of the Central Asian Paleozoic orogenic zone;
中亚古生代造山带成矿作用基本特征
2.
A direct genetic affiliation was speculated upon the formation and evolution of the foreland depression in the northwestern part of the Junggar Basin and the uplifting and thrusting of the West Junggar orogenic zone on the basis of geological, geophysical and geochemical data.
通过大量地质、地球物理和地球化学资料论证 ,笔者认为准噶尔盆地西北前陆坳陷与西准噶尔造山带之间在成因上具有耦合关系 ,即准噶尔盆地西北前陆拗陷的形成、演化与西准噶尔造山带的上隆、推覆之间存在内在成因联系。
3.
Based on the abundant information about every epoch ophiolite s petrochemistry, geochemistry characterictics, which distributed over West Kunlun area, after a detailed field inspect, the author regarded that the ophiolite strip gave so much important information about the tectonic evolution of West Kunlun orogenic zone.
在西昆仑造山带的北侧存在着一条西起盖孜 ,向东经奥依塔格、库地、苏巴什至祁曼塔格的蛇绿岩带。
4) Orogenic belts
造山带
1.
Based on introducing the tectonic facies concept,this paper summarizes the significance of tectonic facies to the studies on tectonic evolution of orogenic belts,non Smith stratigraphy and sedimentary geology in orogenic belts.
在综合介绍国内外关于大地构造相概念和大地构造相研究方法的基础上，综述了大地构造相分析在研究造山带结构和演化、非史密斯地层以及造山带沉积地质学方面的意
2.
The geochemical study of orogenic belts is aimed at reconstructing the tectonicregime of paleo-plates, and discussing the formation, evolution and metamorphism of rocks invarious evolutionary phases and corresopding continental geodynamics as well as deep mantleprocess.
造山带地球化学研究的目标主要是为重建古板块构造格局服务，其次是探讨古造山带不同演化阶段岩石的形成、演化、变质及其所反映的大陆动力学和深部地幔过程。
3.
Follow the policying of "let a hundred flowers blosson and a hundred schools of thought contend", more than ten geologists are invited by the editorial department of "Earth Science Frontiers" to take part in a writing conversation about the study of orogenic belts.
《地学前缘》编辑部遵循"百花齐放，百家争鸣"的方针，以笔谈会形式邀请10多位地质学家从不同角度阐述造山带研究的意义、理论和方法等。
5) Tianshan orogenic belt
天山造山带
1.
The geoscience transect from Korla to Jimsar runs through the northern margin of the Tarim basin, the Tianshan orogenic belt and the southern margin of the Junggar basin.
库尔勒—吉木萨尔剖面横跨塔里木盆地北缘、天山造山带和准噶尔盆地南缘 。
2.
The Tianshan orogenic belt within Chinese territory is situated in the northwestern China.
天山造山带是一个著名的地震活动带，而阴山-燕山断隆带历史上不但没有大地震发生，小地震也不多见，是一个地震空白区。
6) Langshan orogenic belt
狼山造山带
1.
Mineralization response to the structural evolution in the Langshan orogenic belt,Inner Mongolia.;
内蒙古狼山造山带构造演化与成矿响应
补充资料：造山带
| 造山带 orogen 经受强烈褶皱及其他变形而形成的规模巨大的线（带）状大地构造单元。由一定地质历史时期中的活动带演化而成，并相对于稳定的克拉通存在。 地槽学说中的造山带是指一定构造旋回时期的大型长条形活动带（见地槽），在经历先下沉后上升的构造运动、并在强烈构造变形或岩浆活动过程中最后由强烈隆起的造山运动而形成，是地槽演化的终结产物，又称为褶皱带。板块构造学认为，造山带是岩石圈板块的会聚敛合边界（见海沟）上的重要地质标志，也是板块碰撞（见大陆碰撞）的直接产物。造山带的平面分布和走向是随刚性板块边界的形态和碰撞过程的不同而各异 。地质时期中的造山带具有以下特征：①都是强烈构造变形区，其中岩层强烈褶皱断裂，沉积厚度的梯度变化大，多发育大量的浊积岩、混杂堆积、低成熟度的碎屑岩和磨拉石。②沿造山带走向，刚性板块因碰撞有时可出现双变质带；在垂直造山带方向上因板块俯冲消亡，使火山活动的岩石化学组分具一定规律的变化，即由大洋向大陆方向，岩石由拉斑质钙碱系列而变成碱性系列。③造山带中的蛇绿岩套或蛇绿混杂堆积为呈带状分布的无根透镜层状体，并被认为是古洋壳的碎片，是板块碰撞的消减过程中洋壳成楔状断片的残留体，是古海洋关闭消失的证据。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条