1) collision of the Indian to the Eurasian plates 印度欧亚板块碰撞2) India-Eurasia collision 印度-欧亚板块碰撞 1. Numerical simulation of activity of Red-River Fault Zone during India-Eurasia collision; 印度-欧亚板块碰撞期间红河断裂带活动性的数值模拟研究3) Eurasia-India plate collision 欧亚-...
2000a. Numerical simulation of the collision between Indian and Eurasian plates and the deformation of the present Chinese continent [J]. Acta Seismologica Sinica , 13 (1): 1–8.Fu Rongshan,Huang Jianhua,Xu Yaomin, et al. Numerical simulation of the collision between Indian and Eurasian ...
12.The model for the subduction and collision of the Indian plate with the Eurasian plate and its implications for the tectonic evolution of the Qinghai-Xizang Plateau印度板块向欧亚板块俯冲碰撞的新模式及其对青藏高原构造演化的影响 13.Twenty of the 34 papers specialized in deep-seated processes of ...
Balancing shows that there has been a maximum eastwards extrusion of the convergent zone of about 250 km, and that up to 1000 km of shortening has occurred in the Himalayas. -Authors 展开 关键词:Tertiary Paleogene Asia Strike faults Indian Plate Eurasian Plate Plate collision Middle Eocene ...
The relationship of the crustal contact between the Indian and Eurasian plates is a key issue in understanding crustal thickening and the subduction of the Indian lithosphere beneath the Qinghai-Tibetan Plateau. Across the middle of the Yarlung-Zangbo Suture (YZS), we deployed an ∼450-km-long...
In contrary to ocean-continent subduction, the mantle lithosphere is delaminated from the crust as the Indian Plate subducts underneath Eurasia. Existing structural images of the crust and upper mantle of the Tibetan Plateau reveal that there were both northward and southward subductions over ...
Along these lines of logic, recent studies have indicated that the convergence rate between the Indian and Asian continents, together with the magnitude and recycling efficiency of subducted Neo-Tethyan lithosphere, has exerted important controls on the amount of magmatic CO2emissions and thereby global...
That is a point of view that many of mountains in the continent of Chinawere built by a collision of the Indian, Eurasian and Pacific plates. But according to the geology of the ophiolite belts and the sutures in China,during the periods of the closing of paleooceans and suturing, welding...
Evidence ofcontinental collisionis as accessible as the nearest copy of the “Times Atlas.” A glance at the map shows the northern edge of theIndian subcontinentfestooned with mountain chains rising as India crashes northward intoEurasia. The processes ofcontinental crustsubduction and ultrahigh pressu...
the NWW-trending faults in North China and the south part of South China are possibly dominated by the collision of the Indian Plate to the Eurasian Pl... SUO YanHui,LI SanZhong,LIU Xin,... - 《岩石学报》 被引量: 9发表: 2013年 Quantum Dissipation in Open Harmonic Systems: Operator Sol...