| 辽宁排山楼金矿围岩的岩石学特征 |
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| 作者姓名： | MalogoJ.M.Kongola WANGEn-de YUMing-xu MoustafaElOmella |
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| 作者单位： | 东北大学资源与土木工程学院, 辽宁沈阳 110004 |
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| 基金项目： | This study was supported by the China Scholarship Council(GrantNo.160)，National Nature Science Foundation of China(Grant No.400722006)，the Key Task Project of Science and Technology of Liaoning Province(GrantNo.2001230001). |
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| 摘 要： | 排山楼地区变质作用的主要因素为热量(约600℃)、化学活动流体和压力(地压应力和挤压应力).地壳震动是造成本区造山作用的原因.这种现象与板块构造理论相吻合.矿物分异作用序列为:首先,受火成侵入活动的影响,产生片麻岩、糜棱岩、花岗岩;然后,经历地压和挤压的作用;最后,发生各种类型蚀变作用,包括绢云母化、硅化、碳酸岩化、方解石化、绿泥石化、脱氧作用等.排山楼金矿成矿模式可概述如下:a)成矿作用为热液蚀变型,矿床赋存在太古宙变质岩大型韧性剪切带中;b)矿体产于裂隙中;c)矿体形态与岩脉和细脉形态一致;d)围岩经历了强烈的蚀变作用;e)黄铁矿是最重要的富金矿物,热液流体来源于侵入体,在流经破碎带和裂隙带后,在围岩中沉积黄铁矿.主要岩石类型有花岗岩、角闪岩、片岩、片麻岩和糜棱岩.区内广泛发育青盘岩化、泥化和绢云母化蚀变作用.主要蚀变矿物有石英、黄铁矿、白云母、绢云母、绿帘石、黑云母、微斜长石、方解石、角闪石、云母和锆石.矿体主要赋存在花岗岩和片麻岩中.主要蚀变作用为绢云母化、黑云母化、硅化和方解石化.蚀变过程中,铁氧化物(铁帽、云母)覆于贫硫酸盐矿石表面.蚀变类型有青盘岩化(黏土)、泥化和绢云母化.通常,氧化铁与黏土矿物的混合影响卫星影像中光谱的反射.利用遥感技术方法,适于这类矿床的进一步预测研究.
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| 关 键 词： | 金矿 围岩 构造运动 韧性剪切带 蚀变 矿化 |
| 收稿时间： | 2003-12-08 |
PETROLOGIC
CHARACTERIZATION OF GOLD HOST ROCKS:A case study of Paishanlou Gold Mine, Liaoning
Province, China |
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| MalogoJ.M.Kongola WANGEn-de YUMing-xu MoustafaElOmella.PETROLOGIC
CHARACTERIZATION OF GOLD HOST ROCKS:A case study of Paishanlou Gold Mine, Liaoning
Province, China[J].Geology and Resources,2004,13(2):85-95. |
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| Authors: | Abstract |
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| Institution: | Institute of Resources and Civil Engineering, Northeastern University, Shenyang 110004, China |
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| Abstract: | Standard laboratory procedures and remote sensing techniques were employed in the characterization of gold bearing rocks of the Paishanlou area. Results indicate that, the rocks were formed in an alteration complex of medium temperature and pressure. The area was under intense polymetamorphism (ductile shearing, and hydrothermal metamorphism), which occurred along the deformation zone stretching from Jinzhou to Fuxin. The area bears some propylitic, phyllic (or sericitic) and argillic alteration styles. Gold minerals are contained in fine grained pyrite in silicified zones, and associated with metamorphosed Precambrian rocks. The host rock is composed of gneiss, mylonite and trondhjemite granite, and has a distinctive gold lead geochemical affinity. |
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| Keywords: | gold host rocks tectonic movements ductile shearing alteration mineralization |
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