tethys

An Evolution of Tethys in Global Ocean - continent Transformation

全球洋－陆转换中的特提斯演化

Search for new domains of marine origin petroleum : remained Tethys in the northern South China Sea

寻找海相油气新领域&从南海北部残留特提斯谈起

Evolution and basic characteristics of Tethys orogenic zone , western Yunnan

滇西特提斯造山带的演化及基本特征

However , the TOC content is much lower than the black shale in West Tethys .

但是，其有机碳含量与西特提斯相比明显偏低。

Its formation and evolution was controlled by the dynamics of the Tethys tectonic belt .

盆地形成演化受特提斯构造带地球动力学控制。

Preliminary analysis of the Tethys Himalayan tectonic domain

特提斯-喜马拉雅构造域初步分析

Tethyan Geology for 100 Years THE EVOLUTION OF EAST TETHYS

特提斯地质一百年

Mesozoic basins are distributed around Tethys and belong to southern foreland basin zone .

在海相沉积之后接受了陆相沉积，中生代盆地环特提斯洋分布，属南前陆盆地带。

Tectonic Evolution of the Tethys in Southwestern China : Is Controlled by Plume Tectonics

中国西南特提斯构造演化&幔柱构造控制

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

中国西南部特提斯构造域金矿找矿标志及找矿预测

The river that formed these deposits was actually not far from an ancient ocean known as the Tethys Sea .

那条化石所在的河流实际上离古老的海洋T都不远。

This provides strong geochemical evidences for correctly understanding the evolution of the old Tethys and the basin range transition .

从而为正确认识古特提斯洋的演化和盆山转换过程提供了强有力的地球化学证据。

What is the relationship between the Paleo_ Tethys and the Central Orogenic System ?

论东特提斯形成与演化的基本特征（3）古特提斯与中央造山系的关系；

The result shows that there were two different fluid flow areas in " Sanjiang " middle belt during Neo Tethys .

研究表明，三江中段新特提斯阶段区域流体存在两个性质不同的流体作用区域。

The evolution of Tethys can be divided into 5 stages . 1 ) Rifting stage ( P );

特提斯演化可划分为以下5个阶段：1）裂谷起始阶段（P）；

Its formation may be related to the close of the ancient Tethys , and shows the shear convergence characteristics from west to east .

通过对该弧状构造带的构造特征、构造演化及动力学背景进行的探讨，研究认为，其生成可能与古特提斯收缩闭合有关，并呈现出由西向东的剪式闭合特征。

Earthquake along Yangtze river results from the new structural movement which is under the control of both Tethys tectonics and Pacific tectonics .

这一特殊的自然地理面貌严格受青藏地块、秦祁昆地块和扬子板块的构造格局控制，是特提斯构造系统和太平洋构造系统及其二者复合作用的结果。

This is identical with the characteristics of west Guangdong Hainan gold metallogenic belt and the evolution of Tethys tectonics .

这一结果与粤西-海南成矿带的成矿时代特征及特提斯构造演化特点相吻合。

The formation and evolution of this Mesozoic basin may feedback the information about the evolution of the Tethys tectonic zone in Western Yunnan .

兰坪－思茅中生代盆地的形成和演化可反馈滇西特提斯构造演化的信息。

Tectonic Evolution of Mesozoic Basins on the Northwest Pacific Margin and the North Tethys Margin ( I ) .

西北太平洋边缘及特提斯北缘中生代盆地成因（上）

Southeastern China continental margin has undergone a complicated convergence process of the Eurasian plate with the Pacific plate and Tethys plate .

中国大陆东、南边缘经历了欧亚板块与太平洋板块和特提斯板块会聚作用的复杂过程。

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

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。

The Cretaceous-Tertiary Hehuai basin was generated owing to the combined effect of the Tethys and Pacific Ocean dynamic systems .

白垩-第三纪河淮盆地是在特提斯与太平洋动力学体系联合作用下形成的。

Plate convergent margins and island-arc orogenesis in Eastern Tethys

东特提斯板块会聚边缘与岛弧造山作用

Shear convergence of plates and suturing of terranes : a new model for the comsumption of the Meso Tethys

板块剪式汇聚加地体拼贴&中特提斯消亡的新模式

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

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。

Permian-Triassic paleoclimate of Eastern Tethys and its paleogeographic implication

东特提斯地区二叠&三叠纪古气候特征及其古地理意义

In Mesozoic era , the formation and evolution of the Mesozoic Lanping Simao basin were controlled by the Tethys tectonic zone .

在中生代，该盆地的形成与演化受特提斯构造带的控制。

The Cretaceous west of Lancang River is distributed in Gondwana and the small intermontane basin of Tethys orogen .

澜沧江以西的白垩系，分布于冈瓦纳古陆和古特提斯造山带的小型山间盆地，地层层序齐全，岩性、厚度稳定，含古生物化石。

Closing of Tethys and continuous compressing and squeezing of Indian plate were the tectonic dynamics background for the formation of foreland basins in western China .

特提斯洋关闭和印度板块持续推挤是中国西部前陆盆地形成的构造动力学背景。