This is the first report of Triassic Radiolaria within the Yarlung-Zangbo Suture Zone.
这是雅鲁藏布江缝合带三叠纪放射虫的首次报告。
Taoxinghu ophiolite was an important discovery of Longmu Co-Shuanghu suture zone in recent years.
桃形湖蛇绿岩是龙木错-双湖缝合带近期的重要发现。
It proves that the Jinshajiang suture zone could not have formed the main suture zone in the Paleo-Tethys domain.
因此，金沙江带不能作为古特提斯域的主缝合带。
The Huluhe ophiolite zone includes "Early Paleozoic of Yemashan-Mouli-Lajishan suture zone" a eastward extension.
提出葫芦河蛇绿岩带属“野马山—木里—拉脊山早古生代结合带”东延组成部分。
Qiaohuote copper deposit, located at suture zone of Nalati plate, is medium-sized ore related to plate subduction.
乔霍特铜矿床位于那拉提板块缝合带上，是与板块俯冲作用有关的中型矿床。
Guangtoushan granitoids are located in the north of Mianlue suture zone, which consist of tonalites and monzogranites.
光头山花岗岩体出露于勉略缝合带北侧，主要由英云闪长岩和二长花岗岩组成。
Therefore, the superimposed fold system and the suture zone are interrelated in origin and they have the distinct deformation features in di.
叠加褶皱与拼接带具有成生联系，且各自代表了不同构造部位的变形特点。
A lot of geologic records reveal that North Qilian mountains are an early Paleozooic suture zone between the Alashan massif and the central Qilian massif.
大量地质记录揭示北祁连山是介于阿拉善地块和中祁连地块间的一个早古生代缝合带。
Langkazi area lies in the south side of Indian river Brahmaputra suture zone, the north margin of Himalayan flat bar and south margin of Zhada Zhongba flat bar.
浪卡子地区位于印度河—雅鲁藏布江缝合带南侧，喜马拉雅板片北缘和札达—仲巴板片南缘。
It is the Guishan Formation of! the former Xinyang Group that is the strongly deformed pre-Devonian tectono-stratigraphic unit distributed in the main suture zone.
原信阳群龟山组就是沿主缝合带分布的前泥盆纪强应变构造地层体。
Therefore, the superimposed fold system and the suture zone are interrelated in origin and they have the distinct deformation features in different structural positions.
叠加褶皱与拼接带具有成生联系，且各自代表了不同构造部位的变形特点。
The Renbu ophiolitic mélange zone locates in the easternmost middle section of the Yarlung Zangbo suture zone, and there are lots of fresh diabase tectonic block outcrops in the mélange zone.
仁布蛇绿构造混杂带位于雅鲁藏布江缝合带中段之最东部，其间混杂伴生有大量较为新鲜的辉绿岩构造岩块。
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 ;
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；
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