摘要
Habo porphyry Cu(-Mo-Au) deposit, located in west of southern Ailaoshan-Red River Cenozoic metallogentic belt, is a newly-discovered deposit. The Habo intrusion complex cropping out in this district is characterized with multiple intrusions. Based on the lithological and geochemical characteristics of the Habo deposit, the authors in combination with previous research results in this area believe that the alkaline porphyry deposit in eastern Tibet is the extension of Yulong metallogenic belt and the product in a late-collisional transform regime in Eastern Tibet.