西藏地区的地热活动十分强烈,尤以其南部的喜马拉雅地热带为最盛。 喜马拉雅地热带西起克什米尔地区,往东沿印度河进入西藏西部阿里高原,并继续往东越过马攸木山口,沿雅鲁藏布缝合线延伸到东部昌都地区,在横断山脉与我国另一强烈的滇西地热带相衔接。整个地热带绵延逾2000余公里。喜马拉雅地热带的南界大约与喜马拉雅山 The geothermal activity in Tibet is very strong, especially in the southern Himalayas. Himalayan geography west of Kashmir, east along the Indus to enter the western plateau of Ali, and continue east across the Yau wood pass, along the Brahmaputra suture extends to the eastern part of the Qamdo, in the Hengduan Mountains and another strong Yunnan Western tropical convergence. The entire tropical stretches more than 2000 kilometers. The southern boundary of the Himalayan tropics is about the same as the Himalayas