sparked by the slow-motion collision between the Indian and Eurasian tectonic plates that began some 60 million years ago. As India, then an island, ploughed into Eurasia, it buckled the surface, thrusting skyward to form the highest mountains on our planet. ...
S. (1996). Mapping the descent of Indian and Eurasian plates beneath the Tibetan Plateau from gravity anomalies. Journal of Geophysical Research, 101, 11,275-11,290. https://doi.org/10.1029/96JB00531Jin Y, McNutt M K, Zhu Y. Mapping the descent of Indian and Eurasian plates beneath ...
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...
The Himalayan-Tibetan Plateau is currently the world’s largest example of an active continent-continent collisional orogen. The plateau formed primarily due to the collision between the Indian and Eurasian tectonic plates after subduction and closure of the intervening Neotethyan Ocean in the past 55...
The dynamic setting and processes of tectonic and magmatic evolution of the oblique collision zone between Indian and Eurasian plates: Exemplified by the tectonic evolution of the Three River region, eastern Tibet印度-欧亚侧向碰撞带构造-岩浆演化的动力学背景与过程——以藏东三江地区构造演化为例 LIU Jun...
evolution of the oblique collision zone between Indian and Eurasian plates: Exemplified by the tectonic evolution of the Three River region, eastern Tibet印度... LIU JunLai,SONG ZhiJie,CAO ShuYun,... - 《岩石学报》 被引量: 96发表: 2006年 The Moho beneath western Tibet: Shear zones and ec...
The Himalayas, formed due to the collision between Indian and Eurasian plates, is one of the most active interplate regions of the Earth which has witnessed many great and large earthquakes in the recent past. Space–time patterns of seismicity in the Himalayan fault system identified regions of...
The seismic observation shows that the LAB topography is almost sinusoid, implying that the deformation is primarily caused by the end horizontal forces due to the massive continental collision between the Indian and Eurasian plates. 5.2 Presence of Lithosphere-Asthenosphere Boundary Below India [15] ...
But even that formidable death toll was surpassed in a few moments last autumn, when the boundary between the Indian and Eurasian tectonic plates shook, ... None - 《Nature》 被引量: 0发表: 2006年 Farmer suicides in India This paper indicates about farmers suicides in India and also World...
The tectonic evolution of the Indo-Myanmese arc region is dominated by oblique subduction of the Indian plate at the southeastern margin of the Tibetan Plateau[38]. In this area, the ocean-continent collision between the Indian and Eurasian plates along the Sunda arc in Southeast Asia ...