基本释义:

特提斯海

网络释义

1)Western Tethys,特提斯海

2)Paleo-Tethys ocean,古特提斯海

3)Tethyan realm,特提斯域

4)Tethys,特提斯

5)Tethyan ocean,特提斯洋

6)Palaeo-Tethys,古特提斯

用法和例句

Regional fluid charecters and regimes of "Sanjiang" middle belt during Neo-Tethys.;

三江中段新特提斯阶段区域流体的性质与状态

Deri′angma-Xiala section in the Xainza area, Tibet, China:A bridge for the stratigraphic and paleontological correlation between Gondwana and Tethys during the Late Carboniferous and Early Permian;

西藏申扎地区德日昂玛-下拉剖面:冈瓦纳和特提斯晚石炭世—早二叠世地层和古生物对比的桥梁

Relationship Among the Neo-Tethys,Tectonic Diktyogenises and Basins in West China;

中国西部新特提斯洋与构造变格及盆地

It is regarded that paleo-Asian ocean and Tethyan ocean are the main factors controlling sedimentation and structure of the area, that structures.

包括:古亚洲洋和特提斯洋是影响该区沉积和构造的主要因素;塔里木盆地西南坳陷两侧不对称;深浅层次构造差异较大;区内断裂和背斜多形成于喜玛拉雅构造运动。

The north slope area of the Mount Qomolangma being a main component of Tethyan Ocean belongs to Himalayan orogen intermediate on the junction between the northern India plate and Yarlung Zangbo river suture belt.

位于印度板块北缘和雅鲁藏布江结合带之间的珠穆朗玛峰北坡地区,属于喜马拉雅造山带,是特提斯洋的重要组成部分。

The study on the structure, volcanic sediment and magmatism shows that the east Kunlun Mountains belong to the Palaeo-Tethys active continental margin during the Hercynian-Indosinian period.

东昆仑地质构造特征、石炭—三叠系火山 -沉积建造及区域岩浆作用研究显示 ,海西 -印支期 ,该区属于古特提斯北侧活动陆缘的组成部分。