新疆阿尔金山阿北银铅矿控矿构造特征与矿床成因

The Altun mountain of Xinjiang North silver lead ore controlling structure and ore genesis

新疆阿尔金山阿北银铅矿是近年来地质矿产研究工作者在阿尔金山脉东部地区发掘的中型规模的多金属矿床,地理位置夹持在阿尔金山脉不同走向的断裂带之间,阿北银铅矿控矿构造实质上是一种具有韧脆性的断裂破碎带^([1])。本文分析研究了阿北银铅矿控矿构造的基本地质特征和银铅矿多金属矿床的形成原因,能够促进该地区的银铅矿的开采利用进程。

The Altun mountain of Xinjiang North silver lead in recent years of Geology and mineral resources research workers in the polymetallic deposit in medium scale excavation in Eastern Altun Mountains. The geographical position of the holding in the Altun Mountains to different fracture zone, the Ag Pb ore controlling structure is essentially a ductile brittle fracture zone of^（[1]）. In this paper, the basic geological features of the ore controlling structure of the North silver lead deposit and the cause of the formation of the silver lead polymetallic deposit have been studied and analyzed, which can promote the exploitation and utilization of the silver lead ore in this area.