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江西大湖塘北段石门寺钨铜钼矿化关系研究 被引量:8
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作者 叶泽宇 张智宇 +1 位作者 潘小菲 彭花明 《岩石矿物学杂志》 CAS CSCD 北大核心 2016年第3期457-468,共12页
江南造山带中段的赣北大湖塘矿集区是我国近年查明的世界级超大型钨矿产地,并伴生大型铜矿。本文对该区北段石门寺矿区燕山期不同岩石单元的W、Cu、Mo矿化特征与成矿年龄进行了系统研究。白钨矿多呈细脉浸染状产于似斑状花岗岩及其与围... 江南造山带中段的赣北大湖塘矿集区是我国近年查明的世界级超大型钨矿产地,并伴生大型铜矿。本文对该区北段石门寺矿区燕山期不同岩石单元的W、Cu、Mo矿化特征与成矿年龄进行了系统研究。白钨矿多呈细脉浸染状产于似斑状花岗岩及其与围岩的外接触带;黄铜矿与辉钼矿多呈浸染状共生于似斑状黑云母花岗岩、细粒黑云母花岗岩、黑云母花岗斑岩及其围岩中。矿石矿物化学研究表明,似斑状黑云母花岗岩、细粒黑云母花岗岩和黑云母花岗斑岩中的硫化物成分较均一,黄铜矿中Cu 34.215%~35.161%、Fe 29.206%~30.721%、S 34.388%~35.520%,辉钼矿中Mo 59.44%~60.54%、S 40.067%~40.370%;似斑状黑云母花岗岩、细粒黑云母花岗岩、黑云母花岗斑岩和石英大脉中的辉钼矿Re-Os同位素模式年龄均值分别为143.3 Ma、145.2 Ma、144.5 Ma、143.6Ma,在误差范围内基本相同,指示该矿区内的Cu、Mo矿化为一期成矿作用形成,由此给出辉钼矿Re-Os同位素等时线年龄145.1±1.0 Ma (MSWD=0.46),代表Cu、Mo矿化时间。结合前人岩浆岩研究结果,石门寺矿区白钨矿与Cu、Mo矿化是两期成矿作用的产物,前者与似斑状黑云母花岗岩密切相关,而后者可能与燕山晚期黑云母花岗斑岩有成因联系,成矿物质由斑岩向其他岩石单元迁移逐渐成矿。 展开更多
关键词 矿化特征 RE-OS同位素定年 矿石矿物化学 成矿金属来源 石门寺钨铜钼矿
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Chemical, physical, thermal, textural and mineralogical studies of natural iron ores from Odisha and Chhattisgarh regions, India
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作者 Anand Babu KOTTA Swapan Kumar KARAK Mithilesh KUMAR 《Journal of Central South University》 SCIE EI CAS CSCD 2018年第12期2857-2870,共14页
The chemical,physical,thermal and texture properties of iron ores from different regions of Odisha and Chhattisgarh regions,India,have been investigated to understand the compositional variations of Fe,Al2O3,SiO2,S an... The chemical,physical,thermal and texture properties of iron ores from different regions of Odisha and Chhattisgarh regions,India,have been investigated to understand the compositional variations of Fe,Al2O3,SiO2,S and P.They were analyzed for its susceptibility to meet the industrial requirements,for various iron manufacture techniques.Chemical analysis indicated that the majority of the iron ores is rich in hematite(>90wt%),poor in gangue(<4.09wt%SiO2and<3.8wt%Al2O3)and deleterious elements(P<0.065wt%and S<0.016wt%)in all these iron ores found to be low.XRD peaks reviled that the gangue is in the form of kaolinite and quartz,and same was observed in Fourier transform infrared(FTIR)spectroscopy in the range of914to1034cm–1.The iron ores were found to have excellent physical properties exemplify with tumbler index(82wt%–91wt%),abrasion index(1.27wt%–4.87wt%)and shatter index(0.87wt%–1.64wt%).FTIR and thermal analysis were performed to assimilate the analysis interpolations.It was found that these iron ores exhibit three endothermic reactions,which are dehydration below447K with mass loss of0.13wt%to1.7wt%,dehydroxylation at525–609K with mass loss of1.09wt%–4.49wt%and decomposition of aluminosilicates at597–850K with mass loss of0.13wt%–1.15wt%.From this study,we can conclude that due to its excellent physico-chemical characteristics,these iron ores are suitable for BF and DRI operations. 展开更多
关键词 iron ore chemical analysis mineralogy analysis thermal analysis textural analysis
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