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岩浆形成于大陆弧的构造背景,俯冲的陆壳和古特提斯洋壳对富集的源区均有贡献。Both subducted continental and ancient Tethyan oceanic crust contributed to enriched mantle source region.

特提斯构造域是除冈瓦纳构造域、欧亚大陆构造域、太平洋构造域之外的又一全球范围的大构造域。Tethyan realm is a global structural realm on the world besides of Gondwana realm, Euro-Asian realm and Pacific realm.

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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.

喜马拉雅地区的碳酸盐台地产生、发展和消亡与特提斯造山带形成的动力演化息息相关。The initiation, development and termination of the Himalayan carbonate platforms are closely related to the dynamic evolution of the Tethyan orogenic belt.

桂南—粤西的云开地块,位于特提斯构造带和环太平洋构造带的交汇处。The Yunkai Block, extended in southern Guangxi and western Guangdong, is located in the intersection area of the Tethyan and the circum Pacific tectonic zones.

中国南方是全球特提斯巨型油气富集带的组成部分,原始沉积提供有丰富的烃源。The southern China is a part of the hydrocarbon-enriched belt of the Tethyan region, where abundant hydrocarbon resources were supplied with the primary deposits.

研究表明羌塘盆地在油气资源的许多方面可与中东特提斯油气集聚区相类比,因而成为中国油气资源战略选区的首选目标之一。Comparable with the Middle East petroleum provinces in the Tethyan domain, the Qiangtang Basin is selected as the target area for the oil and gas resources in China.

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成矿物质主要来源于特提斯向环太平洋构造域转换后闽西南地区晚侏罗世-早白垩世壳源花岗岩浆。And the mineralization material originated from late Jurassic granite magma in the southwestern Fujian formed after transformation from the Tethyan to Pacific domain.

特提斯成矿域仅出露于青海的南部,三江成矿区的北段以中新生代成矿为特点。The Tethyan metallogenic domain consists mainly of north Sanjiang metallogenic belt located in southeast Qinghai-Tibet plateau, with middle Cenozoic being the major metallogenic period.

该套地层的发现填补了微陆块上二叠系地层的空白,对古特提斯多岛洋研究具有重要意义。The discovery has filled the gap in the studies of the Permian system occurring in micro-landmass and is significant to the researches of numerous oceanic islands in the ancient Tethyan.