与其具有相似构造背景的西亚特提斯带盆地群是目前世界上油气最富集的地区。
The basin swarm of the West Tethys belt, which is the richest petroleum-bearing region in the world presently, has a similar tectonic setting to the Qiangtang basin.
在中生代，该盆地的形成与演化受特提斯构造带的控制。
In Mesozoic era, the formation and evolution of the Mesozoic Lanping Simao basin were controlled by the Tethys tectonic zone.
盆地形成演化受特提斯构造带地球动力学控制。
Its formation and evolution was controlled by the dynamics of the Tethys tectonic belt.
自地中海经土耳其、伊朗、喜马拉雅山到缅甸、印尼群岛的特提斯汇聚碰撞带，显示为低速异常链。
The low velocity anomaly chain is located along the convergence belt of Tethys from Mediterranean Sea, Turkey, Iran, Himalayan orogens, Burma, Indonesian Islands.
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。
This is identical with the characteristics of west Guangdong Hainan gold metallogenic belt and the evolution of Tethys tectonics.
火山岩岩浆的形成既与古特提斯洋的俯冲洋壳在深部脱水有关，又与南澜沧江带红层盆地形成初期的拉张作用有关，为山—盆转化阶段特殊岩浆类型。
The origination of the magma is related with the dehydration of the subducting plate of the Palezoic Tethy Sea and the early tension of the form of the Lancangjiang belt red layer basin.
洋岛玄武岩以弄槐枕状熔岩为代表性火山岩，原为古特提斯洋盆中的夏威夷型洋岛，现保存在印支期前陆褶皱冲断带的一个外来岩席中。
The oceanic island basalt is represented by the Nonghuai pillow lava, which is, originally Hawaii type one in the Paleotethyan ocean, an allochthon in the Indosinian foreland fold and thrust belt.
古亚洲与特提斯构造交汇带盆地群发育石炭系、侏罗系（中下统）、白垩系（下统）等多套烃源岩，具有厚度大、分布广、有机质丰度高的特点。
A number of suites of Carboniferous, middle-lower Jurassic and lower Cretaceous hydrocarbon source rocks were developed in the basin groups in the Paleo-Asian and Tethyan structural confluence area.
以上认识为中、越交界地区构造上属古特提斯造山带提供了新证据，为重塑该地的古特提斯演化提供了重要资料。
The knowledge provides new testimonies for the area bordering China and Vietnam being, tectonically, Paleotethysides and key data for reconstructing Paleotethyan evolution there.
因此，金沙江带不能作为古特提斯域的主缝合带。
It proves that the Jinshajiang suture zone could not have formed the main suture zone in the Paleo-Tethys domain.
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.
提出二叠纪时期冈底斯带可能为一个在古特提斯洋盆中呈条块状“漂浮”的冈瓦纳碎片。
They propose that during the Permian the Gangdise belt might be a fragment of Gondwana that floated in the Paleo-Tethyan Ocean.
研究表明，冈瓦纳的裂散、亚洲的增生和特提斯构造带的演化都受控于星球级纬向构造体系。
Study indicates that Gondwana dispersion, Asian accretion and geological evolution of the Tethyan tectonic belt were controlled by the global latitudinal tectonic system.
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.
由此本文认为麻扎-康西瓦-苏巴什结合带经历了震旦-早志留世的原特提斯洋的演化和中泥盆世-早三叠世的古特提斯洋的演化；
Therefore, this paper thought that Mazha-Kangxiwa-Subashi suture zone experienced Sinian to Early Silurian evolvement of Proto-Tethys and Devonian to Early Triassic evolution of the Palaeo-Tethys ;
由此本文认为麻扎-康西瓦-苏巴什结合带经历了震旦-早志留世的原特提斯洋的演化和中泥盆世-早三叠世的古特提斯洋的演化；
Therefore, this paper thought that Mazha-Kangxiwa-Subashi suture zone experienced Sinian to Early Silurian evolvement of Proto-Tethys and Devonian to Early Triassic evolution of the Palaeo-Tethys ;
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