Meso - Tethys a sea lying between Laurasia and Gondwana during the Middle and Late Mesozoic.

中特提斯是中生代中晚期存在于南、北大陆之间的海洋.

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.

Qiangtang Basin is a large residual basin in the Tethys tectonic region formed in late - Paleozoic - Mesozoic.

西藏羌塘盆地是特提斯构造域巨型油气富集带中一个大型晚古生代 - 中生代海相残留盆地.

It is concluded that northward subduction of the Neo-Tethys resulted in the magmatic eruption of the Yeba Formation in the Early-Middle Jurassic time.

叶巴组火山岩形成于岛弧或活动大陆边缘的构造环境，其动力来源应为新特提斯洋向北的俯冲消减。

The plate collision helped close the western part of the ancient Tethys Sea and lifted up the massive European mountain chain that persists today.

同时，这次板块碰撞封闭了特提斯海（即古地中海）的西部，并且形成了仍保存至今的欧洲大部分山脉。

In the waters of the prehistoric Tethys ocean, a sinuous, 50-foot-long beast with gaping jaws and jagged teeth died and sank to the seafloor.

史前特提斯海洋水域，一条50英尺长，张着血盆大口，满嘴锯齿状牙齿的怪兽，盘桓着，缓缓倒下，沉入海底。

The Cassini spacecraft snapped this shot in February as it swooped past Calypso, which trails behind the larger moon Tethys in roughly the same orbit around Saturn.

这张照片是在今年2月份，卡西尼号宇宙飞船从卡里索普上方快速飞过时拍摄到的。卡里索普星的轨道在土星第二大卫星特提斯的后方，二者围绕土星旋转的轨道大致相同。

Based on the late Paleozoic fold basement, Simao Triassic sedimentary basin formed in the early continental-island arc collusion stage after the close of Paleo-Tethys ocean.

三叠纪沉积盆地建立在晚古生代褶皱基底之上，形成于古特提斯洋闭合后，造山早期的弧陆碰撞阶段。

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。

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。