A large concentration of ore deposits (ie, tungsten, tin, lithium, beryllium, lead, zinc, silver,
antimony and gold) related to metamorphism and hydrothermal activity of granite developed …

Abstract The Tibetan Plateau geographically contains internal and external drainage areas
based on the distributions of river flows and catchments. The internal and external drainage …

西藏亚东-谷露裂谷带是新生代的活动构造带, 具有构造活跃, 地震频繁, 热泉广布,
大地热流高等特征, 孕育了丰富的地热资源. 已实现商业开发多年的羊八井地热田和羊易地热田 …

Abstract The Yarlung River flows between the east-trending Himalayan and Gangdese
orogens, and across several north-trending rifts. It carries rich information on the Indian …

Abstract The Tibetan Plateau was formed by long-term terrane accretion and block collision,
controlled by complicated Mesozoic-Cenozoic geodynamic mechanisms. However, its detail …

We present a comprehensive geochronological, mineralogical, and geochemical study on
previously unknown olivine leucitites occurring in the Maiga area of southern Tibet to …

Located in the eastern Himalaya and surrounded by Yalaxiangbo dome, the Cona Woka rift
may provide valuable information for the extensional mechanism of crust and distribution of …

Active graben systems in south Tibet and the Himalaya are the surface expression of
ongoing east–west extension, although the cause and spatiotemporal evolution of normal …

Precise studies of Quaternary extension rates across NS‐trending normal faults in southern
Tibet are important to understand the recent tectonic evolution of the high plateau. As one of …

Highlights•Buzhu Au orogenic gold mineralization controlled by Himalayan crustal uplifting
processes•Mineralization occurring as the hydrothermal system transitioned from the …