| 中国青藏高原特提斯的形成与演化 |
| |
| 引用本文： | 潘裕生,方爱民.中国青藏高原特提斯的形成与演化[J].地质科学,2010,45(1). |
| |
| 作者姓名： | 潘裕生 方爱民 |
| |
| 作者单位： | 中国科学院地质与地球物理研究所,北京,100029 |
| |
| 基金项目： | 中国自然科学基金项目 |
| |
| 摘 要： | 青藏高原的形成是特提斯演化的结果。本文根据区域大地构造演化和沉积学证据,将青藏高原特提斯在时间上划分为3个阶段,即早期、中期和晚期。早期从震旦纪开始至奥陶—志留纪结束,这个阶段的大洋我们称作"原特提斯"。中期从泥盆纪开始至石炭—二叠纪结束,通常称这个大洋为"古特提斯"。晚期从二叠纪末、三叠纪初开始一直延续到第三纪早期,这个阶段的大洋通常被称作"新特提斯"。在空间上,青藏高原特提斯可以划分为3个区域相,即北区、中区和南区。上述3个阶段完全可以与空间上的3个区域相对应,原特提斯主要发育于北区,大洋消亡后的遗迹残留在青藏高原第5缝合带中,即西昆仑—阿尔金—北祁连缝合带。古特提斯主要发育于中区,大洋消亡后的遗迹残留在青藏高原第3、4缝合带中,即金沙江缝合带和昆仑南缘缝合带。新特提斯主要发育于南区,大洋主洋盆消亡后的遗迹残留在青藏高原第1缝合带中,即雅鲁藏布江缝合带,它的弧后盆地消亡后的遗迹残留在第2缝合带中,即班公湖—怒江缝合带。
|
| 关 键 词： | 形成与演化 特提斯 青藏高原 构造带 |
Formation and evolution of the Tethys in the Tibetan Plateau |
| |
| Pan Yusheng,Fang Aimin.Formation and evolution of the Tethys in the Tibetan Plateau[J].Chinese Journal of Geology,2010,45(1). |
| |
| Authors: | Pan Yusheng Fang Aimin |
| |
| Abstract: | The Tibetan Plateau is closely related to the evolution of Tethys,and it constitutes the main scope of the eastern Tethys.According to current data from regional tectonic studies and sedimentary records,Tethys in Tibetan Plateau can be divided into three different stages,namely,Neo-Tethys,Paleo-Tethys,and Proto-Tethys,representing the Tethys in MesozoicCenozoic,Late Paleozoic and Early Paleozoic,respectively.Furthermore,they correspond to three zones in the Tibetan Plateau,namely the northern Tethyan,the central Tethyan region and the southern Tethyan region,respectively.The Proto-Tethys lies in Kunlun and Qilian Mountains in the northern Tethyan region.represented by the Fifth Suture Zone as its remnant.It had been formed in Sinian and closed in Ordovician and Silurian.It was the earliest Tethyan ocean known up to now.The Paleo-Tethys lies in Hoh Xil-Bayan Har in the central of Tibet Tethyan.represented by the Third and Fourth Suture Zones.It initiated as a back-arc basin in Ordovician and eventually formed as a basin typical oceanic crust in Carboniferous and Permian due to its continuous back-arc breaking and spreading.The Paleo-Tethys ocean still existed until the end of the Triassic.The Neo-Tethys lies in the southern Tethyan region,represented by the Yarlung Zangbo Suture Zone.It initiated on the shelf in the northern part ot Gondwanaland at the end of Permian and the beginning of Triassic and formed in Mesozoic and Cenozoic.It began to subduct northward and was consumed very soon at the end of Jurassic,however,the main oceanic basin,which is represented by the Yarlung Zangbo Suture Zone and named Neo-Tethys,didn't consume until Early-Mid Eocene.It is obvious that the Tethyan ocean moved southward step by step according to the space distribution pattern of major Tethyan oceans in different periods.The evolution of Tethys,combined with the characteristics of terranes and distribution pattern of biogeography,also indicates the plate tectonic model that the Tibetan Plateau was formed by the continuous rifting of Gondwanaland and the accretion of the Eurasia. |
| |
| Keywords: | Formation and evolution Tethys Tibetan Plateau Suture zone |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
|
