特提斯构造域

鄂尔多斯西缘及邻区是中国东部滨太平洋构造域和西部特提斯构造域两大构造动力体系的转换枢纽带。

Western Ordos region and its adjacent area is the geological & geophysical divide or transform hinge between circum-Pacific tectonic domain in eastern China and Tethyan tectonic domain in western China .

中国西南部特提斯构造域金矿找矿标志及找矿预测

Au ore searching marks and metallogenic prediction in Tethys tectonic realm of the southwest China

在特提斯构造域研究方面，大陆岩石圈的构造演化及其地球动力学机制一直受到地学界的普遍关注。

The continental lithospheric tectonics and geodynamics in the Tethyan domain are conspicuous by the frontiers of modern earth sciences .

燕山期以后，华南形成的构造格局为：扬子&特提斯构造域及太平洋构造域。

After the Yanshan movement , the tectonic framework formed in South China is the Yangtze Tethys structural domain and the Pacific structural domain .

东亚西太平洋分为3个区域地幔对流与地表的西太平洋构造域、古亚洲构造域和特提斯构造域相吻合。

The three regions of mantle convection beneath East Asia and the Western Pacific are in agreement with Western Pacific , Paleo-Asiatic and Tethyan tectonic domains .

云南位于喜马拉雅－特提斯构造域与滨太平洋构造域的复合部位，地质构造十分复杂，新生代火山岩浆活动激烈。

Yunnan is located in the composite part of the Himalayan-Tethys structural domain and the circum-pacific structural domain , with very complicated geological structures and intensive Cenozoic volcanic magmatism .

闽西南地区是特提斯构造域向环太平洋大陆边缘构造域转换的典型地区，区内多期构造演化形成了复杂多变的构造单元格局和多种成岩成矿环境。

Southwest Fujian is a typical transitional area from Tethyan tectonic regime to Pacific epicontinental tectonic regime . The complex tectonic framework and varied rock_forming and ore_forming environments resulted from multiple_episode tectonic evolutionary processes .

四川盆地是特提斯构造域巨型油气富集带中一个大型古生代中新生代海相陆相叠合盆地，其形成与演化受特提斯构造域与滨太平洋构造域控制。

The Sichuan Basin , a large Paleozoic and Meso-cenozoic era marine and continental basin , is situated between Tethys tectonic domain and marginal Pacific tectonic domain , which control its formation and development .

喜马拉雅运动期源自特提斯构造域的强大挤压应力使北天山快速、大幅度隆升，并向盆地冲断，在盆地南缘发育了陆内造山型类前陆坳陷。

Himalayan movement originated from powerful compressive stress in Tethys tectonic domain , which caused north Tianshan mountains to quick and extensive uplift and thrusting toward Junggar basin followed by shaping foreland depression of intracontinental orogenic type developed in the southern margin of Junggar basin .

滨里海盆地与塔里木盆地不仅同处于特提斯构造域的北缘，中新生代有着十分相似的构造和沉积发育史，而且其古生代的盆地演化、含油气性更具有可比性。

Not only both the Caspian Basin and the Tarim basin are located in the northern margin of Tethyan tectonics and have similar history of structural and sedimentary development during the Meso-Cenozoic , but also they show comparability of the Paleozoic basinal evolution and hydrocarbon-bearing characteristics .

大块的造礁珊瑚，有盘旋的和沟回的表面。中二叠世&新近纪新特提斯洋构造域旋回。

Massive reef-building coral having a convoluted and furrowed surface . ( 3 ) MiddlePermian-Neogene extension-compression cycle of Neo-Tethys .

昌宁孟连构造带位于特提斯喜马拉雅构造域三江褶皱带，是研究和解决该问题的最为关键的地区之一（刘本培等，1993；崔春龙，1999）。

The Changning-Menglian belt , located the drape belt of three river in structure territory of Tethyan-Himalayan , is the one of most pivotal areas which is redounded to research and resolve the problem .

主要褶皱时代在滨太平洋区是晚侏罗世至中始新世，在特提斯大地构造域和内陆区是中晚始新世之交。

The principal fold age is from the Late Jurassic to the Middle Eocene in the Peri-Pacific region and is between the Middle and Late Eocene in the Tethys geotectonic domain and the intracontinental region .

特提斯-喜马拉雅构造域初步分析

Preliminary analysis of the Tethys Himalayan tectonic domain

该区地质历史以来经历了特提斯&喜马拉雅构造域和环太平洋构造作用域的相互转换。

During geological history , this area has experienced the Transformation from Tethyan-Himalayan tectonic domain into circum-Pacific tectonic domain .

综合以上资料及前人的研究成果认为，康西瓦构造带是分隔古亚洲和特提斯两大构造域的右行走滑转换构造带。

Based on above data and previous study KSTB is regarded as a right-hand shove transform tectonic belt which divides the paleo-Asian tectonic domain and the Tethys domain .

摘要：尕龙格玛铜多金属矿床位于特提斯-喜马拉雅构造域的东段，冈瓦纳古陆与欧亚古陆强烈碰撞、挤压地带。

Abstract : Galonggema Cu-polymetal deposit is located in the eastern of the Tethys-Himalayan tectonic domain , which is the strong collision and extrusion zone between Gondwana and Eurasian ancient land .

鄂尔多斯盆地地处中国沉积盆地分布的中带，兼受东滨太平洋构造域和西南特提斯-喜马拉雅构造域的影响，是我国第二大含油气盆地。

Ordos is the secondary petroliferous basin located at the middle zone of sedimentary basin in china , affected by The East Pacific tectonic process and The Southwest Tethys-Himalayas tectonic process .

金矿床（点）主要分布在华北地台、扬子地台和特提斯三大构造成矿域中。

The gold ore deposits are mainly distributed in the north China platform , Yangtz platform and Tethys , the three tectonic-metallogenic realms .