The Xizang Plateau, the principal component of the Qinghai-Xizang Plateau, is the youngest and highest plateau in the world. It is also one of the most intensive earthquake regions in China. Researching of earthquake ...
supported by the National Natural Science Foundation of China(Grant Nos.41174070,41474088,41274063);China National Special Fund for Earthquake Scientific Research in Public Interest(Grant Nos.201308011,201008001);the Scientific Investigation of the April 14,2010 M7.1 Yushu,Qinghai Earthquake
Polarization analysis of teleseismic data has been used to determine the XKS(SKS,SKKS,and PKS)fast polarization directions and delay times between fast and slow shear waves for 59 seismic stations of both temporary an...
During the last 40Ma the marine 87 Sr/ 86 Sr record shows a rapid rise (from 0 7078 to 0 7092) [1] , a trend which has been linked to the Himalayan Orogeny [2] . Indeed, many Himalayan rivers, principally those of the...
River Yamuna is one of the most polluted rivers of the India. It originates from Yamunotri glaciers in the lower Himalayas at an elevation of approximately 6387 meters. The barrages formed on the river are playing a m...
The Kulu\|Rampur and Larji windows in the western Himalaya make a window in window structure in the Lesser Himalaya between the Main Boundary Thrust (MBT) and Main Central Thrust (MCT). The former constituted of late ...
Most carbonatites occur in relatively stable, intra\|plate areas but some are found to occur in near to plate margins and may be linked with plate separation (Woolley, 1989). Although many carbonatites have been disco...
TheNationalNaturalSciencesFoundationofChina (No .49732 10 0 )andNationalKeyProject (No .19980 40 80 0 )forBasicResearchofTibet
The Eastern Himalayan Syntaxis (EHS) is one of the strongest deformation area along the Himalayan belt resulted from the collision between Indian plate and the Eurasian plate since 50~60Ma, and has sensitivity tracke...
The western boundary of the Eastern Himalayan Syntaxis (EHS) is a deformation belt up to 30km wide (Fig.1). Trending ca. N35°E, it separates the Gangdise magmatic belt in the west from the gneiss of EHS in the east. ...