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花敖包特铅锌银矿床是近年来新发现的位于大兴安岭南段西坡银多金属成矿带上一重要矿床。自2000年通过土壤地球化学测量与激电测量发现本矿床以来,相继对该矿床进行了一系列地质基础理论研究以及有效勘查,包括通过各种地质方法揭示矿体成矿规律、探查矿体控制要素,运用物探勘查技术(高精度磁测、瞬变电磁法以及激电测量等)、化探勘查技术(土壤地球化学测量以及深穿透地球化学技术等)以及三维地质建模技术对矿区深部及其外围进行勘查,取得了一些新的认识,通过这些勘查研究显示本矿床在深部和外围仍具有良好的成矿前景。
The Ovootite Pb-Zn-Ag deposit is an important deposit newly discovered in recent years in the Xipo silver-polymetallic metallogenic belt in the southern section of Daxinganling. Since the discovery of the deposit by geochemical and electrical measurements in 2000, a series of geological basic theoretical studies and effective prospecting have been carried out on the deposit successively, including revealing ore-forming rules through various geologic methods and exploring ore body control Elements, the use of geophysical prospecting techniques (high-precision magnetic, transient electromagnetic and electrical measurements, etc.), geochemical exploration techniques (geochemical surveying and deep-penetrating geochemical techniques, etc.) and three-dimensional geological modeling of deep mining And its periphery, some new understandings have been obtained. According to these exploration studies, the ore deposit still has good prospecting potential in the deep and periphery.