| 平度市新河铁矿地质特征分析 |
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| 引用本文： | 田晓留,黄玉华,梅西华,杨冲.平度市新河铁矿地质特征分析[J].山东国土资源,2015,31(8). |
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| 作者姓名： | 田晓留 黄玉华 梅西华 杨冲 |
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| 作者单位： | 山东泰山地质勘查公司;山东泰山地质勘查公司;山东泰山地质勘查公司;山东泰山地质勘查公司 |
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| 摘 要： | 平度市新河铁矿位于安丘莱州铁成矿带中部，铁矿床产于古元古代粉子山群小宋组中，共圈定3个磁铁矿体，矿石为石英型磁铁矿石，属沉积变质型铁矿床。赋矿层位具专属性，以磁异常为其找矿标志，通过综合分析研究，认为该铁成矿带内具有较好的找矿前景。
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| 关 键 词： | 铁矿 沉积变质型磁异常 地质特征 安丘莱州铁成矿带 平度新河 |
Analysis on Geological Characteristics of Xinhe Iron Deposit in Pingdu City |
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| TIAN Xiaoliu,HUANG Yuhu,MEI Xihua and YANG Chong.Analysis on Geological Characteristics of Xinhe Iron Deposit in Pingdu City[J].Land and Resources in SHANDONG Province,2015,31(8). |
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| Authors: | TIAN Xiaoliu HUANG Yuhu MEI Xihua and YANG Chong |
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| Abstract: | Xinhe iron deposit is located in middle part of Changyi Laizhou iron metallogenic belt in Pingdu city. The iron deposit occurred in Palaeoproterozoic Xiaosong formation of Fenzishan group. Three magnet ore bodies have been circled totally. Ore bodies are quartz magnetite, and belong to sedimentary metamorphic type. The orebearing layers have specialization. Magnetic anomaly is considered as prospecting criteria. Through comprehensive analysis and research, it is regarded that iron metallogenic belt has a good prospecting potentiality in this area. |
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