【摘要】 新疆阿尔恰勒铅锌矿位于塔里木板块伊犁亚板块察布查尔—伊什基里克山裂谷带中,矿体受地层层位控制,产状及围岩基本一致,呈似层状赋存于下石炭统阿克沙克组灰岩中,后期构造及岩浆侵入对矿化富集有重要改造作用,阳起石化蚀变可作为矿区铅锌矿体最直接的找矿标志。根据矿区矿化富集规律及地质、地球物理和地球化学勘查成果,认为该区具有中—大型铅锌矿找矿潜力。更多还原

【Abstract】 Aerqiale lead-zinc ore deposit located in Qapqal –Yishijilike Mountain rift valley in Yili inferior plate. The ore-bodies occurrence was the same as surrounding rock. The later period structure activity and magma intrusion reformed the ore bodies, which made it being more enrichment. Actinolitization rock alteration is the direct prospecting indicator. Combined with the regularity of mineralization, geophysical prospecting and geochemical prospecting,it is considered that there is great potentialities in prospecting for mid-large scale lead-zinc ore deposit in Aerqiale ore area.更多还原