文章摘要
冯健行,许海娃,冯源,赵泽龙,冯乐.内蒙古白音查干铅锌银矿地质特征及找矿方向分析[J].矿产勘查,2022,13(6):737-746
内蒙古白音查干铅锌银矿地质特征及找矿方向分析
Analysis on geological characteristics and prospecting direction of the Baiyinchagan Pb-Zn-Ag deposit in Inner Mongolia
投稿时间:2021-02-04  
DOI:10.20008/j.kckc.202206004
中文关键词: 白音查干  地质特征  化探异常特征  铅锌银矿床  勘探工程
英文关键词: Baiyinchagan  geological characteristics  geochemical anomaly characteristics  lead-zinc-silver deposit  exploration engineering
基金项目:
作者单位
冯健行 内蒙古亿诚地质矿产勘查开发有限责任公司锡林郭勒盟分公司, 内蒙古 锡林浩特 026000 
许海娃 内蒙古第四 水文地质工程地质勘查有限责任公司, 内蒙古 通辽 028000 
冯源 内蒙古第四 水文地质工程地质勘查有限责任公司, 内蒙古 通辽 028000 
赵泽龙 内蒙古亿诚地质矿产勘查开发有限责任公司锡林郭勒盟分公司, 内蒙古 锡林浩特 026000 
冯乐 黑龙江交通职业学院,黑龙江 哈尔滨, 150000 
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中文摘要:
      内蒙古白音查干铅锌银矿目前已发现多条矿体,矿体受断裂构造控制,呈脉状产出,矿石具浸染状、细脉网脉状结构,矿物组合为典型的中低温矿物组合,说明白音查干铅锌银矿属于中低温热液矿床。但前人对已发现矿体中矿物的标型特征研究较少,对地球化学测量结果的高温元素组合研究薄弱,根据矿物标型特征研究结果,闪锌矿从浅部向深部Fe含量增高,颜色变深;磁黄铁矿仅在底部矿体中出现,呈板状晶型;锡石亦只在底部矿体中见到,呈短柱状晶体。根据1∶10000地球化学测量结果统计分析,Pb、Zn、Ag、W、Mo、Sn元素异常均具有内带,浓集中心明显,而且W、Sn、Mo异常套合较好,与前缘元素异常吻合,推测矿区深部很可能存在W、Sn、Mo高温矿体,是进一步找矿的方向。
英文摘要:
      At present, many ore bodies have been discovered in the Baiyinchagan lead-zinc-silver deposit in Inner Mongolia. Ore bodies are controlled by fault and appear as vein-like occurrence. The ore show dissemination structure and vein-like network, which indicate it belongs to low-medium temperature hydrithermal ore deposit. However, there are few studies on the typomorphic characteristics of minerals in discovered ore bodies, and study of high-temperature elements from geochemical survey is weak. According to research results of mineral typomorphic characteristics, content of Fe in sphalerite increases from shallow to deep, and color becomes darker. Pyrrhotite only occurs at the bottom of ore body and show as plate crystal. Cassiterite is also only found at the bottom ore body, which show as a short columnar crystal. According to the statistical analysis of 1∶10000 geochemical survey results, anomalies of Pb, Zn, Ag, W, Mo and Sn elements all have inner zones, and concentration center is obvious. Moreover, anomalies of W, Sn and Mo are well nested, which are consistent with the anomalies of front elements. It is speculated that there may be high-temperature W, Sn and Mo orebodies in the deep of ore area, which is the direction of further prospecting.
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