英语释义

1. orogeny

片语

orogenic sediment造山运动沈积物

orogenic belt[地质] 造山带

orogenic batholith造山成因的巖基

orogenic arc造山弧

Orogenic deposit造山型

orogenic plateau造山的高原

orogenic crumpling造山挤压作用

英汉例句

• the basic tectonic framework of nw china is an assemblage of several cratonic blocks pieced together with orogenic belts.

  中国西北地区是以若干克拉通为基础，通过造山带拼合形成的盆地山脉省。

• the tectonic movement that occurred since the neogene has been the major developmental and evolutional stage of the latest global crustal deformation and orogenic movement.

  新近纪以来的构造运动是全球最新的地壳形变和造山运动的发展演化阶段。

• this theory could not explain the composition, structure and evolution of continental lithosphere and continental orogenic belt, and also is not in line with modern scientific theory.

  上述理论阐明不了大陆巖石圈、大陆造山带的组成，结构与演化，也与当代的基础理论不尽吻合。

• the tectonic evolution of collisional orogenic belts is studied in detail and corresponding tectono-metallogenic units and metallogenic provinces and belts are distinguished.

  详细地研究了碰撞造山的构造演化过程，划分了相应的成矿构造单元和成矿区带。

• mountains produced by the orogenic movement in the mesozoic time and plateaus formed thereafter by tectonic uplift become an important factor that influences the global climate.

  中生代造山运动造就的山脉和其后由构造隆升形成的高原，也是影响全球气候的主要因素之一。

• the altay orogenic belt, in xinjiang, china was formed mainly during late devonian to early permian and was mainly a thrust-nappe-detachment orogenesis.

  阿尔泰造山带主要形成于晚泥盆世至早二叠世的主造山期，为一沖断-推覆-滑脱的造山作用。

• intracontinental subduction (c-subduction) was the intrinsic cause of circulation of mass flow and energy flow in type-c foreland basins and type-c orogenic belt (thrust belt).

  陆内（c-型）俯沖是c-型前陆盆地与c-型造山（沖断）带物质流和能量流循环的内在原因；

• so-called world a stone, is the best orogenic material.

  号称天下第一石，是造山的绝佳材料。

• the exhalation-spout type deposits of the early paleozoic era and the orogenic type deposits of the late paleozoic to early mesozoic era are the most important deposit groups.

  早古生代时期的喷气喷流型矿床组合和晚古生代—早中生代时期的造山型矿床组合最为重要。

• the tectonic features of the tongbai - dabid orogenic belt are presented in detail based on the geometry and mechanical models for a two -sided orogen.

  从双侧造山带的几何学和力学模式出发，详细地讨论了桐柏—大别造山带的构造特征。

• the orogenic types were controlled by the relative motion mechanism between lithosphere and asthenosphere .

  板块和软流圈之间不同的相对运动机制是形成不同类型造山作用的主要原因。

• different metamorphic types reveal different tectonic conditions and record the evolutionary history and geodynamic process in altai hercynian orogenic belt of xinjiang.

  不同的变质作用类型代表了不同的大地构造环境，记录了造山带的演化历史和动力学过程。

• based on diverse developing evolution stage and orogenic character in east guizhou area, the architectural facies in three developing evolution stage are built up in this region.

  根据黔东地区不同的发展演化阶段和造山性质，建立了该区三个发展演化阶段大地构造相特征。

• a stable area of continental crust that has not undergone much plate tectonic or orogenic activity for a long period.

  大陆地壳长时期内未受到板块构造的或造山活动的很多影响的稳定区。

• in early and middle jurassic, as orogenic activity intensified, the basin subsidence increased and it sediment supply was sufficient.

  早、中侏罗世造山活动强烈，盆地沉降幅度大，物源供应充足；

• sequence stratigraphy will be encountered with new challenges from continental dynamics of archipelago arc orogenic models and multi mechanism uplifting models.

  多岛弧造山模式和多机制的隆升模式等大陆动力学问题也是层序地层所遇到的新挑战。

• there are great bifurcations as yet on the structural environment and on the evolution of the xingmeng paleozoic orogenic belt in southeast inner mongolia during the carboniferous period.

  内蒙古东南部古生代造山带在石炭纪时期的构造环境和构造演化，至今在认识上存在较大的分歧。

• formation of the basin is closely relative to the development of the south dabashan-dahongshan orogenic belt.

  盆地的形成与南大巴山—大洪山造山带的发育密切相关。

• this structural system was formed in the pre - sinian , probably related to the grenville orogenic event.

  这一构造系统形成于前震旦纪，可能与格林威尔造山运动相当。

• in mesozoic, the proterozoic sulu fold belt has undergone orogenic activization resulting in the intrusion of numerous granite bodies with broad development of metasomatic rocks.

  在中生代，苏鲁元古褶皱带受造山作用的影响活化，导致许多花岗巖体的侵入，使交代巖广泛发育。

• the region belongs to a complex intracontinental orogenic belt.

  构造复杂，是典型的陆内造山带发育地区。

• these corresponding relation of highs is related to contacting relation between kuche foreland fill and tianshan orogenic wedge.

  这种高点的对应关系与库车前陆充填及天山造山楔的接触关系有关。