| 云南墨江镍金矿床主要控矿因素分析与研究 |
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| 引用本文： | 方维萱,胡瑞忠,谢桂青,漆亮,苏文超.云南墨江镍金矿床主要控矿因素分析与研究[J].矿物学报,2001,21(1):80-88. |
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| 作者姓名： | 方维萱 胡瑞忠 谢桂青 漆亮 苏文超 |
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| 作者单位： | 中国科学院地球化学研究所矿床地球化学开放研究实验室, |
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| 基金项目： | 国家重大基础研究规划项目! ( 19990 43 2 0 0 )，国家杰出
青年科学基金项目!( 4 992 5 3 0 9)，云南省院校科技合作项目!
(YK980 0 |
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| 摘 要： | 采用控矿因素分析研究，通过构造岩石地层及构造变形筛分探讨镍金矿床的成矿过程，认为本区金镍矿主要为地层及构造控矿。在矿床内，热（泉）水喷溢构造（成矿构造）有似环状粘土岩化带及热水同生沉积－交代－喷流构造岩石层序，脆－韧性剪切带（储矿构造）由近水平的纵张裂隙构造、左行共轭剪切裂隙及相对封闭的脆韧性剪切带组成。脆性张剪性X形微裂隙系统为富金矿脉的定位提供了构造空间。成矿演化过程为：①晚泥盆世热水同生沉积成岩成矿期形成含金黄铁矿硅质岩；②印支期逆冲推覆型脆韧性剪切构造成岩成矿期形成含金脆韧性剪切带；③燕山－喜马拉雅山期深源热流体叠加成矿期形成富金矿脉。指出3处成矿远景区，认为红土型金矿很可能是本区一种新的金矿类型，值得重视研究。
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| 关 键 词： | 墨江 镍金矿床 控矿因素 储矿构造 成矿过程 云南 矿床地质 围岩蚀变 |
| 文章编号： | 1000-4734（2001）01-0080-09 |
| 修稿时间： | 2000年7月17日 |
RESEARCH AND ANALYSIS ON ORE-CONTROLLING FACTORS FOR MOJIANG-YUANJIANG NICKEL-GOLD DEPOSITS IN YUNNAN, CHINA |
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| Fang Weixuan,Hu Ruizhong,Xie Guiqing,Qi Liang,SU WenChao.RESEARCH AND ANALYSIS ON ORE-CONTROLLING FACTORS FOR MOJIANG-YUANJIANG NICKEL-GOLD DEPOSITS IN YUNNAN, CHINA[J].Acta Mineralogica Sinica,2001,21(1):80-88. |
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| Authors: | Fang Weixuan Hu Ruizhong Xie Guiqing Qi Liang SU WenChao |
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| Abstract: | Based on research and analysis on ore-controlling factors and analysis of tectono-lithostratigraphic units to shed light on Ni-Au metallogenic processes, it is suggested that the main ore-controlling factors for the Mojiang-Yuanjiang Ni-Au deposits in Yunnan Province include strata-controlling and tectonics-controlling. In the Mojiang-Yuanjiang Ni-Au mine, the Upper Devonian Jinchang Formation consists of low-grade metamorphic volcano-sedimentary rocks formed in a deep-water, volcanic-related hydrothermal depositional basin. This Formation is composed of slate, chert, palimpsest siltstone and sandstone interbeded with tuff mudstone, volcanic lava and tuff. Three tectono-lithostratigraphic units (the Lanshan, Sishibaliangshan and Mahudong) can be recognized in the Jinchang Formation. The Lanshan unit (D3jy1) was formed by volcanism and volcanic-related hydrothermal deposition and is referred to as the volcanic-exhalative-genetic unit. Nickel-gold-bearing pyritic cherts in the Mojiang deposit occur in the lower part of the Lanshan rock-unit, ranging in age from 358±8.6 (2σ) Ma (Sm-Nd isochron dating) to 354.7±0.72 (2σ) Ma (Rb-Sr isochron dating). The Sishibaliangshan unit (D3jy2) consisting of slate, chert, palimpsest siltstone and sandstone, volcanic lava rock and tuff, is also referred to as the volcanic-exhalative-genetic unit. The Mahudong unit (D3jy3) is composed mainly of a suite of fine-grained turbidite rocks with acidic volcanic lava and violet-red sandstones at its top.
The ring-like clayized zone and the tectono-lithostratigraphic sequence of hydrothermal deposits are located at hydrothermal-water vents that are one of the main ore-host structures. The Yanshanian brittle-ductile shear zones that are another main type of ore-host structures are typified by the proximately horizontal tension cracks, sinistral shear fractures, close-off brittle-ductile shear zones, and Cr-illite was formed at 178 Ma to 76 Ma. The Himalayan brittle tension cleavages are the best ore-host structures for high-grade Au orebodies. The Mojiang Ni-Au deposits probably underwent four main Ni-Au metallogenic epochs. Firstly, Ni-Au-bearing pyritic cherts may be formed by volcanic-related hydrothermal deposition in Late Devonian. Secondly, the Ni-Au-bearing ductile shear zones were perhaps formed at the end of Permian or at the beginning of Early Triassic. Thirdly, the Au-bearing brittle-ductile shear zones were perhaps formed by thrust-nappe-type shear tectonics during the Yanshanian orogeny. Finally, deep-source hydrothermal fluids in the Himalayan orogen may superimpose the high-grade Au orebodies. Much attention should be paid to the laterite-type gold deposits as a new prospecting target in the future. |
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| Keywords: | Mojiang Ni\|Au deposit ore\|controlling factor metallogenic process ore\|hosting structure Yunnan |
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