广西砂子岭银多金属矿矿床地质特征及成矿规律  

Geological characteristics and metallogenic regularity of Shaziling silver polymetallic ore deposit in Guangxi Province

作　　者：周星[1] 梁景规 龙鹏[1] 严新泺[1] 张厚云[1] 江沙[1] 黄桂强[1] 

机构地区：[1]中国冶金地质总局广西地质勘查院,广西南宁530022 [2]广西第六地质队,广西贵港537000

出　　处：《矿产与地质》2016年第6期934-939,共6页Mineral Resources and Geology

基　　金：广西容县砂子岭矿区银铅锌矿详查项目(2011-2013年)

摘　　要：本文通过区域地质背景、矿区地质特征概况、矿床地质特征的分析研究,总结矿区内银多金属矿床的成矿规律。结果表明,矿体展布主要受石英斑岩的断层破碎带构造控制;石英斑岩体为银矿体的主要矿源体;石英斑岩岩浆的侵入在粉砂岩、含泥粉砂岩与角闪黑云石英二长岩体沉积接触的地质界面中,这种封闭构造环境中利于富集形成高品位的银矿石;矿化富集用与不同构造的交叉、构造形变强度、岩石破碎强度以及蚀变交代强烈程度等因素密切相关。可将石英斑岩的断层破碎带及接触蚀变带作为银多金属矿找矿方向。石英斑岩断层破碎带中的硅化、黄铁矿化、褐铁矿化、绿泥石化蚀变,是该区银矿找矿的一种地表直接标志。In this paper, the metallogenic regularity of Ag-polymetallic deposit in the mining area is summarized through the analysis of the regional geological setting, geological characteristics of the mining area and deposit geology features. The result shows that the orebody distribution is mainly controlled by the fault broken zone of quartz porphyry, and that the quartz porphyry is the main source of silver orebody. For the intrusion of quartz porphyry magma in the geological boundary between silty sandstone, argillaceous silty sandstone and hornblende-biotite-quartz monzonitic granite, the high-grade silver ores are formed in this closed tectonic environment. The mineralization enrichment is closely related with the crossing of different structures, the structural deformation intensity, the rock crushing strength and the alteration and replacement intensity and other factors. The fault zone and contact alteration zone of quartz porphyry can be used as the prospecting direction of silver polymetallic ore deposit. Silicification, pyrite mineralization, limonitization and chloritization alteration in the fault zone of quartz porphyry are all the direct surface signs of silver mineralization exploration in the area.

关 键 词：石英斑岩 成矿规律 银多金属矿 找矿方向 砂子岭 

分 类 号：P618.4[天文地球—矿床学] P618.52[天文地球—地质学]