| 福建马坑铁（钼）矿床矽卡岩矿物学特征及分带研究 |
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| 引用本文： | 张志,张承帅.福建马坑铁（钼）矿床矽卡岩矿物学特征及分带研究[J].岩石学报,2014,30(5):1339-1354. |
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| 作者姓名： | 张志 张承帅 |
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| 作者单位： | 中国地质大学, 北京 100083;中国地质调查局发展研究中心, 北京 100037;中国地质科学院矿产资源研究所, 北京 100037 |
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| 基金项目： | 本文受国家“973”项目（2012CB416800）和国家自然科学重点基金项目（40930419）联合资助. |
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| 摘 要： | 马坑大型铁(钼)矿赋存于莒舟-大洋花岗岩体外接触带黄龙组(C2h)灰岩和林地组(C1l)碎屑岩层间构造破碎带中,铁矿与矽卡岩密切共生,但矿床成因尚存在争议。本文就马坑铁矿矽卡岩进行了矿物学特征研究。电子探针分析结果表明:该矿矽卡岩矿物组合主要为辉石、石榴子石和钙蔷薇辉石,退化蚀变岩矿物组合为角闪石、绿帘石、绿泥石、石英等。单斜辉石以透辉石和钙铁辉石为主,仅存在少量锰钙辉石;似辉石为钙蔷薇辉石和蔷薇辉石;石榴子石端元成分以钙铁榴石为主,钙铝榴石少量;角闪石属于钙角闪石,矿物学特征表明它们形成于相对较氧化的条件下。马坑铁矿的矽卡岩是由热流体沿灰岩与碎屑岩之间层间构造破碎带交代形成的,铁矿石大部分产于矽卡岩内,磁铁矿多稍晚于矽卡岩,不仅广泛交代矽卡岩,而且还直接交代灰岩、砂岩等围岩,呈交代结构;主矿体下盘常出现厚层石英岩,碎屑岩也出现了明显的交代,矽卡岩分带现象普遍,与典型矽卡岩矿床特征一致。结合矿床地质特征,马坑铁矿矿床类型应为层控矽卡岩型矿床。
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| 关 键 词： | 矽卡岩 分带 电子探针分析 层控 马坑铁(钼)矿床 |
| 收稿时间： | 2013/10/10 0:00:00 |
| 修稿时间： | 1/2/2014 12:00:00 AM |
Skarn mineral characteristics and zonation of the Makeng Fe-Mo deposit in Fujian Province |
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| ZHANG Zhi and ZHANG ChengShuai.Skarn mineral characteristics and zonation of the Makeng Fe-Mo deposit in Fujian Province[J].Acta Petrologica Sinica,2014,30(5):1339-1354. |
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| Authors: | ZHANG Zhi and ZHANG ChengShuai |
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| Institution: | China University of Geoscience, Beijing 100083, China;Development and Research Centre, China Geological Survey, Beijing 100037, China;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China |
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| Abstract: | The Makeng Fe-Mo deposit is a large deposit hosted in the interlayer fracture zone between carbonates of Huanglong Formation (C2h) and clastic rocks of Lindi Formation (C1l) at the exo-contact zone of the Juzhou-Dayang granite. The iron ore are closely coexisting with skarns. However, the ore genesis here has still been controversial. In this paper, we studied the mineralogical characteristics of skarns in Makeng Fe-Mo deposit with electron microprobe analysis, which showed that the mineral assemblages of skarns in this deposit mainly consisted of pyroxene, garnet and bustamite. The retrograde altered minerals were comprised of chlorite, epidote, amphibole and quartz. The mineral composition of clinopyroxene are diopside, hedenbergite, and a small amount of johannsenite. Pyroxenoids are mainly composed by bustamite and rhodonite. The end member of garnet is dominated by andradite, with minor grossularite. The amphibole in this deposit can be classified into calcic amphibole. All the mineralogical characters of skarns showed that they were mainly formed under relative oxidizing conditions. The skarns in Makeng Fe-Mo deposit resulted from the metasomatism formed by thermal fluid flowing along the interlayer fracture zones between limestone and clastic rocks, most iron ore hosted in the skarns, usually the magnetites formed later than the skarns and constituted a metasomatic texture, not only replaced skarns widely, but also direct alternated limestone, sandstone in the wall rock; the footwall of main orebody often appeared thick quartzite, furthermore the metasomatic also appeared obvious in clastic rocks. The skarn zonations were widespread in the deposit, consistent with typical skarn-type ore deposits. Combining the geological features with mineralogical characteristics of skarns in the Makeng Fe deposit, it shows that the deposit is a strata-bound skarn-type deposit. |
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| Keywords: | Skarn Zonation Electron microprobe analysis Strata-bound Makeng Fe-Mo deposit |
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