摘要
阿尔哈达铅锌矿主要产于泥盆系的NW向断裂破碎带中，矿体具雁行排列、局部交叉产出的特征，以盲矿体为主；成矿早期可能以岩浆热液（399-407℃）为主，而中、晚期的热液以大气降水或混合水（194-287℃）为主；硫分别来源于岩浆热液、沉积地层和大气降水；铅同位素测试结果则显示了成矿（岩）物质的混源特点。矿床为与岩浆热液有关的受断裂控制的中温热液铅锌（银）矿。
Arhada Pb-Zn deposit occurs mainly in cataclastic zone of Devonian System and ore bodies are dominated by blind ones in en echelon and locally cut with each other. Magmatic fluid （399-407℃） dominated the ore-forming stage and meteoric water or mixed fluid （194-287℃） is dominant in middle, late stages. Sulfur was derived from sedimentary strata and meteoric water. Pb isotope composition shows multiple sources of ore materials. It is a magmatic hydrothermal fluid-related and cataclastic fracture-controlled mesothermal Pb-Zn deposit.
出处
《地质找矿论丛》
CAS
CSCD
2006年第B10期70-73,共4页
Contributions to Geology and Mineral Resources Research
