The research on ore-controlling factors of Haxiyatu iron-polymetallic deposit of East Kunlun

Abstract

Haxiyatu iron-polymetallic deposit of East Kunlun is located in Qimantage met allogenic belt, the main met allogenic elements are iron, copper, lead, zinc, gold, etc. Based on the geological characteristics and mineralization of ore deposits, this paper concluded that, firstly the brittle contact zone of Jinshuikou rock group and carbonate rock provided a good space for mineralization, secondly the deep minor fractures caused by the regional fracture provided the transport channel for the material. At last, the quartz diorite originated from the mixed source of crust-mantle in the mining area provided a material basis for the mineralization.