中国非金属矿工业导刊Issue(6)：23-29,7.
柴北缘青龙滩硫铁矿床地质特征及找矿模型
Geological Characteristics and Prospecting Model of Qinglongtan Pyrite Deposit,Northern Margin of Qaidam Basin
XIE Tong-peng 1LI Jian 1WANG Xian-zhen1
作者信息
- 1. The First Geological Exploration Institute of Qinghai Province,Haidong 810600,China||Qinghai Engineering Research Center of Deep Exploration Technology for Large and Ultra-large Gold Deposits around Qaidam Basin,Haidong 810600,China
- 折叠
摘要
Abstract
The Qinglongtan pyrite deposit is situated within a significant metallogenic belt along the northern margin of the Qaidam Basin,characterized by superior metallogenic geological conditions.Although extensive exploration and research have been conducted previously,studies on the evolutionary model of the metallogenic system and integrated prospecting prediction models remain insufficient.This study systematically analyzes the geological characteristics of the deposit,constraints on metallogenic epochs,and multi-stage mineralization processes,combined with structural-lithofacies mapping and geophysical anomaly features.A composite metallogenic model of"volcanic exhalative sedimentation-tectonic modification-skarn superposition"is proposed.Through comprehensive analysis of geological,geophysical,and alteration indicators,a multi-factor prospecting model is established,focusing on key elements including"NW-trending fault-controlled mineralization,ore-hosting volcanic sequences,coupled magnetic-induced polarization anomalies,and greenschist-skarn alteration assemblages."The research outcomes not only deepen the understanding of regional pyrite mineralization mechanisms but also provide novel methodological guidance for the exploration of analogous deposits.关键词
柴北缘青龙滩硫铁矿床/热水喷流沉积/构造—热液叠加/成矿模式/找矿模型Key words
northern margin of the Qaidam basin,Qinglongtan pyrite deposit/hydrothermal exhalative sedimentation/tectonic-hydrothermal superposition/metallogenic model/prospecting model分类
天文与地球科学引用本文复制引用
XIE Tong-peng,LI Jian,WANG Xian-zhen..柴北缘青龙滩硫铁矿床地质特征及找矿模型[J].中国非金属矿工业导刊,2025,(6):23-29,7.
