1. 江西省地质局第一地质大队
2. 江西省找矿突破勘查技术中心
3. 中国地质大学(武汉)资源学院
纸质出版:2025
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况二龙, 陈志康, 周江涛, 等. 江南造山带中段七宝山钴铅锌矿床Co赋存状态及地质意义[J]. 地质科技通报, 2025,44(6):61-76.
况二龙, 陈志康, 周江涛, et al. 江南造山带中段七宝山钴铅锌矿床Co赋存状态及地质意义[J]. Bulletin of Geological Science and Technology, 2025, 44(6): 61-76.
况二龙, 陈志康, 周江涛, 等. 江南造山带中段七宝山钴铅锌矿床Co赋存状态及地质意义[J]. 地质科技通报, 2025,44(6):61-76. DOI: 10.19509/j.cnki.dzkq.tb20240410.
况二龙, 陈志康, 周江涛, et al. 江南造山带中段七宝山钴铅锌矿床Co赋存状态及地质意义[J]. Bulletin of Geological Science and Technology, 2025, 44(6): 61-76. DOI: 10.19509/j.cnki.dzkq.tb20240410.
钴(Co)是一种重要的战略性矿产,其赋存状态是当前国际矿床学研究的热点之一。七宝山钴铅锌矿床位于江南造山带中段,矿体受高岽山背斜核部次级褶皱控制、呈NE向透镜状或似层状展布。但目前该矿床钴的赋存状态研究薄弱。对不同中段矿石开展扫描电镜-能谱(SEM-EDS)和电子探针(EPMA)矿物成分分析,结果表明Co主要赋存在斜方砷钴矿、辉砷钴矿、方钴矿和硫镍(铜)钴矿等独立钴矿物中,少量以类质同象形式进入细粒黄铁矿和斜方砷镍矿晶格。斜方砷镍矿幔部常被斜方.砷钴矿交代,边部被辉砷钴矿和辉砷镍矿交代;辉砷钴矿和硫镍(铜)钴矿也常沿黄铜矿边部交代。研究确定早期成矿流体砷活性较高,形成斜方砷镍矿、斜方砷钴矿和方钴矿;随着成矿流体砷活性降低,硫活性增加,晚期形成辉砷钴矿和硫镍(铜)钴矿。该矿床的钴镍矿物交代结构及组合与典型“五元素脉”型矿床具有一定的相似性。因此,七宝山矿床应为具有“五元素脉”特征的热液脉型钴矿床。
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