新疆吐木亚-帕西木金成矿带地质特征及成矿规律  

Geological Characteristics and Metallogenic Regularity of the Tumuya-Paximu Gold Metallogenic Belt in Xinjiang

作　　者：李兴 LI Xing(Institute of Geology and Mineral Exploration,Xinjiang Nonferrous Geolorgical Bureau,Urumqi 830000,China)

机构地区：[1]新疆有色地质勘查局地质矿产勘查研究院,新疆乌鲁木齐830000

出　　处：《甘肃冶金》2024年第3期130-133,共4页Gansu Metallurgy

摘　　要：吐木亚-帕西木金成矿带属昆仑成矿省,是新疆和田地区一条重要的金成矿带。为做好成果转化,提高找矿效率,本文从成矿带地质特征及典型矿床入手,对控矿构造、赋矿岩石、地球化学特征等方面进行剖析,推测出金矿成矿机制,并提出找矿标志,认为韧性剪切带向东为今后找矿重点区域部位。The Tumuya-Paximu gold mineralization belt belongs to the Kunlun metallogenic province and is an important gold mineralization belt in the Hotan area of Xinjiang.In order to do a good job in converting achievements and improving the efficiency of mineral exploration,this article starts with the geological characteristics of the mineralization zone and typical deposits,analyzes the controlling structures,ore bearing rocks,geochemical characteristics,and other aspects,infers the mechanism of gold mineralization,proposes prospecting indicators,and believes that the eastward direction of the ductile shear zone is the key area for future mineral exploration.

关 键 词：金成矿带 成矿规律 地质特征 

分 类 号：P618.51[天文地球—矿床学]