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讨论了砂砾岩型铅锌矿床的形成环境及其地质特征,概述了该类矿床的成矿时代及其空间分布规律;分析了矿床成因的地下水搬运模式、热卤水成矿模式等;建议在古生代以前的古陆边缘及不整合面之上寻找海相砂岩型矿床,在中生代以后的内陆盆地边缘的碎屑岩建造中寻找陆相砂砾岩型矿床。 相似文献
84.
SEDEX型矿床成矿流体的研究是矿床地球化学研究的重要课题之一。正确识别系统中不同的流体来源及其混合过程,是深刻理解SEDEX型矿床形成演化的关键。系统总结了国内几个典型的SEDEX型矿床同位素研究成果,认为B和Si同位素是根据SEDEX型矿床独特的矿物组合而提出的一种示踪方法,对矿床成因和沉积环境示踪效果理想;He、Ar同位素则因为在地壳和地幔储库中有极不相同的组成,是理想的幔源流体示踪剂。鉴于SEDEX型矿床含有电气石、黄铁矿、硅质岩等特殊的矿物与岩石组合,B、Si、He-Ar同位素可能更适合SEDEX型矿床矿化流体来源研究,并指出其理论发展的薄弱之处。 相似文献
85.
ZHU Xiaoqing 《中国地球化学学报》2005,24(4):306-315
Experimental studies were undertaken on leaching of sedimentary rocks ( dolomite and sandstone) and Hg, Sb ores by distilled water under the condition of a completely open system (room temperature and room pressure). The aim is to find whether the halogen elements or metal elements first enter the solution at the early stage of meteoric waters converting to groundwaters and ore fluids, and, at the same time, to understand how and when they enter distilled water solutions from the rocks. The experimental resuhs have shown that F and Cl began to enter the fluids in the initial period of thirty days. With increasing leaching duration, the amounts of the elements that entered the fluids increased steadily. During the period from 120 days to 150 days the amounts increased more drastically, followed a slow increase. It is found that the capability of Cl entering the solutions is much greater than that of F. Hg and Sb were found not to have entered the solutions till 120 days later. During this period of time the pH value of the solutions began to drop. As for Hg and Sb ores, Hg and Sb began to enter the solutions on the 60th or 90th day, greatly ahead of schedule, but the two metallic elements in the rock samples began to enter the solutions 150 days later. Relatively speaking, Hg is more easily leached out than Sb from the rocks. In some rock samples, Sb could be detected in the solutions at the end of the experiment. However, Cu, Pb and Zn had not been detected in the leaching solutions from the beginning to the end of the experiment. In the whole leaching process the pH value of the solutions tend to decrease slowly from 7.1 at the beginning to 6.5 at the end. That is to say, in the interaction between pure water and rock the halogen elements in the rocks were preferentially leached out and then entered the fluids. With increasing water/rock reaction duration and amount of halogen-group elements in the solution and with decreasing pH value of the solution, some active metallic elements began to release in small amounts. This experimental result can explain the source and mechanism of volatile components and trace metals in underground waters. Meanwhile, as for those ore deposits produced by ore fluids derived from meteoric waters, the experimental result is also helpful to the understanding of the geochemical variation trend at the initial stage of conversion of meteoric waters to ore fluids. 相似文献
86.
Wood textures in Jinman copper deposit in western Yunnan and their genetic implications 总被引:2,自引:0,他引:2
Jinman vein copper deposit in western Yunnan occurs in a salt-bearing red clastic rock formation composed of sandstone, siltstone
and shale. Wood texture is considerably developed in the ores. The metallic minerals making up the wood textures mainly include
pyrite, chalcopyrite and bornite. Studies on the samples and examination of their micrographs and electron micrographs have
confirmed that they belong to xenoxylon, reflecting that the ore-hosting rock series is the product of sedimentation in the
terrestrial environment. Organic geochemistry and sulfur and carbon isotopic composition data indicate that the formation
of the deposit is substantially related with underground hot brines and biological processes. 相似文献
87.
金属矿床中卤素元素参与了金属元素的活化,迁移互沉淀成矿的全过程,然而,除F能作为萤石和云母类矿物的组成部分有时富集于矿石中外,Cl,Br,I很难在矿石中富集。在成矿过程中尤其在成矿孤后期,它们能在矿体上部形成范围较广的卤素扩散晕,在茶洞矿床,这种上部扩散晕范围可达200米,其中以I扩散范围最大,Br扩散晕在距矿体50-130米的范围内最明显,Cl扩散晕在距矿体30-110米范围内最明显,卤素元素的这种变化特点,一方面可用来解释成矿热液的演化过程,另一方面可用来作为勘查深部隐伏矿体的地球化学标志,成矿流体中卤素元素与金属元素的配合物着成矿条件的改变而不断被破坏,金属元素作为硫化物等矿物的组成部分沉淀下来,随着热液蚀变的发生和进行,部分瞄卤素元素被带入蚀变带,大部分仍残留在流体相,在成矿的后期,和残余热液一道,以排泄和渗透等方式,在矿体上方或残余热液流经的途中形成大范围的异常。 相似文献
88.
白云鄂博矿区广泛分布着元古代非造山岩浆岩。主要岩性是粗面岩、镁铁钠闪石-长石岩、钾质流纹岩、英安岩、流纹岩、石英斑岩和中长玄武岩,并有大量高钾辉绿岩脉(墙)出露。这些非造山岩浆岩来源于地幔,它们的ε_(Sr)(t)值都较低,ε_(Nd)(t)主要集中在4.52~5.88,钕模式年龄T_(DM)~(Nd)集中在1.54~1.92 Ga。它们的Nd同位素组成和钕模式年龄都与矿石一致,意味着成矿物质来源于这些岩浆岩。这些岩浆岩的锆石U-Pb年龄为1.8 Ga年左右。各种研究结果表明矿床是与非造山岩浆岩有关的热液交代白云鄂博群的产物。 相似文献
89.
张乾 《矿物岩石地球化学通报》1997,(2)
改造成矿作用的定义、类型及特点张乾(中国科学院地球化学研究所,贵阳550002)关键词改造成矿作用改造型矿床类型划分成矿特点改造作用作为一种重要的地质作用,是涂光炽六七十年代经过大量的研究,于80年代正式提出的成矿作用术语。改造成矿作用从根本上解决了... 相似文献
90.