河北省涿鹿县杏园矿区矿床成因及找矿标志  

Ore genesis and prospecting indicators of the Xingyuan mining area in Zhuolu County,Hebei Province

作　　者：谢建平[1] 冯宝山[1] 王艳辉[1] 牛英杰[1] 王自力[1] 韩志伟 刘铭涛[1] XIE Jianping;FENG Baoshan;WANG Yanhui;NIU Yingjie;WANG Zili;HAN Zhiwei;LIU Mingtao(Tianjin North China Geological Exploration Bureau,Tianjin 300170,China)

机构地区：[1]天津华北地质勘查局,天津河东300170

出　　处：《吉林地质》2024年第1期16-22,共7页Jilin Geology

基　　金：天津华北地质勘查局勘查项目(项目编号:TJHK2012B07)。

摘　　要：本研究通过系统的地质、地球化学及地球物理分析,深入探讨了河北省涿鹿县杏园矿区的成矿背景、矿床特征及其找矿指标。利用先进的地质勘查技术,首次明确揭示了矿区内斑岩型与热液脉型矿床的共生关系及其空间分布规律,提出了新的成矿模型和勘查方向。研究结果不仅深化了对杏园矿区成矿规律的理解,而且对指导未来的地质勘查工作,推动矿产资源的合理开发与利用具有重要意义。This study conducts a thorough investigation into the ore genesis background,deposit characteristics,and prospecting indicators in the Xingyuan mining area of Zhuolu County,Hebei Province,through systematic geological,geochemical,and geophysical analysis.Employing advanced geological exploration technologies,it for the first time clearly reveals the symbiotic relationship and spatial distribution patterns between porphyry and hydrothermal vein deposits within the mining area,proposing new metallogenic models and exploration directions.The research results not only deepen the understanding of the metallogenic rules in the Xingyuan mining area,but also have important significant for guiding future geological exploration work and promoting the rational development and utilization of mineral resources.

关 键 词：杏园矿区 成矿机理 斑岩型矿床 热液脉型矿床 成矿模型 

分 类 号：P618.2[天文地球—矿床学]