特提斯喜马拉雅

特提斯喜马拉雅白垩纪层序地层分析

Sequence stratigraphy of the Cretaceous strata in the Tethyan Himalayas

从宽角地震数据得出的特提斯喜马拉雅南部的速度结构

Structural Elements of the Southern Tethyan Himalaya Crust from Wide Angle Seismic Data

藏南特提斯喜马拉雅带中段二叠纪&白垩纪的火山活动（Ⅰ）：分布特点及其意义

Permian to Cretaceous volcanic activities in the central segment of the Tethyan Himalayas ( I ): distribution characteristics and significance

特提斯喜马拉雅二叠纪白垩纪中基性火山岩研究进展

Sm and Nd isotopic geochemistry of Paleo-Mesoproterozoic meta-basic volcanics from Middle Hainan , China ADVANCES ON THE STUDY OF INTERMEDIATE-BASIC VOLCANIC ROCKS FROM PERMIAN TO CRETACEOUS IN TETHYAN HIMALAYA

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 .

在野外实地考察和追索的基础上，详细厘定了特提斯喜马拉雅带中段晚古生代以来火山岩的分布特点和迁移规律。

Based on field investigation and tracing , the authors have defined in detail the characteristics of distribution and migration of volcanic rocks since the Late Paleozoic in the central segment of the Tethyan Himalayan belt .

特提斯-喜马拉雅构造域初步分析

Preliminary analysis of the Tethys Himalayan tectonic domain

义敦岛弧碰撞造山带是特提斯-喜马拉雅巨型造山带中的一个复合造山带。

The Yidun arc collision-orogenic belt is a composue orogenic belt of the giant Tethys-Himalaya orogenic zone .

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 .

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 .

这些进展突出地表现为在世界各地都有新的矿床、矿点发现，其中特提斯&喜马拉雅成矿带有可能成为一条新的铂族元素成矿带。

Even new localities distributed all over the world , it is more attractive that there are some important new discoveries in the Tethys-Himalayan metallogenic belt , suggesting that it is possible for this belt to become a new producer of PGE in the future .