新疆觉罗塔格-黑鹰山成矿带铁（磷）矿找矿远景分析

摘要

通过对新疆觉罗塔格地区进行地球物理特征及含铁（磷）杂岩体地质特征分析，证明古老地台区均有基性－碱性杂岩带存在，这些区带本身就是最有远景的成矿区带。成矿区主要位于地台边缘，受深大断裂控制。觉罗塔格地区与已知的内生铁（磷）矿对比，具有成矿构造条件相同、同时都有杂岩体分布、有磁异常等相同的特征，证明该区具有良好的铁（磷）矿找矿前景。%　　The research of geophysical signature and iron(phosphorus)-bearing complex rock features in Jueluotag district proved that there was basic-alkali complex rock belt in ancestral platform, which was the metallogenic belt most qualified metallogenic prospect. The metallogenic belt is located on the platform margin, controlled by discordogenic fault. Comparing with known endogenic iron (phosphorus) deposit, Jueluotag district has the same structure conditions and the features of complex rock distribution and magnetic anomaly, which proves there are good iron (phosphorus) metallogenic prospect in this district.