摘要
太平川钼铜矿床位于大兴安岭西北部得尔布干成矿带北段,钼铜矿体主要产于蚀变花岗闪长斑岩中。沿北西向断裂上侵就位后,受区域构造影响形成网脉状系统。矿体呈厚板状,连续性好,埋藏浅,已经具备大型矿床格架。通过近几年的找矿勘查与综合研究发现,太平川钼铜矿具有斑岩型矿床的特征,找矿潜力巨大。文章在总结矿床地质、地球化学、地球物理特征的基础上,分析了找矿前景。
Taipingchuan Mo- Cu deposit locates in the northern part of Derbugan metallogenic belt, and the northwest of Da Hinggan Ling. Mo - Cu orebody lies in altered granodiorite porphyry. After up - intrusion displacement along NW trending faults, af- fected by the regional structure, formed net - vein system; ore body characterized by the thick tabular, good continuity, shallow burial, and a large - scale deposit is on the horizon. After ten years of exploration and scientific research, Taipingehuan Mo - Cu deposit has the character of porphyry deposit and considerable prospecting potential. The author proposed prospecting potential based on the geolog- ic, geochemical and geophysical features in the paper.
出处
《矿产勘查》
2011年第6期681-689,共9页
Mineral Exploration
