豪威夫星河矿山矿床地质特征与深部找矿预测

The Geological Characteristics and Deep Prospecting Forecast to Howev Xinghe Mine

豪威夫星河矿区地处欧亚板块与印度板块缝合线东侧,地史上其构造岩浆活动强烈,矿产资源丰富。以豪威夫星河矿区为研究对象,从地质概况、地球化学、矿体岩性、蚀变特征等方面对该区矿床矿体地质特征进行详细研究,研究结果表明其矿床的成因以低温热液型为主。结合高精度磁物探方法,发现矿体明显受地层、构造与岩浆岩控制,同时对可能存在隐伏矿体的深部岩体形态特征及有利成矿条件进行了推断,建议未来可进一步靠大密度的深部钻探验证。

The area of Howev Xinghe Mine is located in the eastern side of the suture line between the Eurasian plate and the Indian plate.In the history of the earth,its tectonic magmatism is strong and its mineral resources are rich.Based on Howev Xinghe mining area as the research object,a detailed study is made from geology,geochemistry,ore body lithology and alteration features of ore deposit geological characteristics of ore bodies in the area.The research results show that the origin of the deposit is mainly low-temperature hydrothermal type.Combined with high precision magnetic exploration method,it founds that the ore bodies are obviously controlled by strata,structures and magmatic rocks,as well as the possible of concealed ore body in deep rock mass morphological characteristics,and favorable metallogenic conditions are concluded to suggest the future with further deep drilling verification by the large density.