桂西隆林-西林锑金矿集区成矿控制因素探讨

华南锑成矿省锑资源储量占全国83%以上,位于成矿省西南部的滇黔桂锑矿带是华南锑成矿省的重要组成部分。文章以滇黔桂锑矿带中部桂西隆林-西林锑金矿集区为例,系统分析了区内82个矿床(点)的赋矿层位、赋矿围岩岩性、容矿构造特征及锑、金矿床共伴生关系,结合3个典型矿床调查及岩浆岩时空分布,探讨锑成矿作用与碎屑岩、岩浆岩的成因联系。研究结果表明:具有高锑背景值的炭质泥页岩和富黄铁矿砂岩是研究区锑成矿的有利岩性,为锑成矿提供了物质来源。岩浆作用对锑成矿既可以起到直接作用(Sb和S来源)也可以起到间接作用(热源),两者均有利于锑矿床的形成。容矿构造分析显示研究区经历了印支期南北向挤压,随后叠加中晚侏罗世北西—南东向挤压。北西西—南东东向和北东—南西向断裂及其交汇处是有利的容矿空间。隆林-西林矿集区锑、金矿床统计显示,区内以独立的锑、金矿床为主,暗示研究区锑、金成矿流体可能多为不同来源流体。在上述研究基础上,文章提出桂西隆林-西林锑金矿集区勘查有利区域:新州背斜核部下泥盆统郁江组炭质泥页岩和富黄铁矿粉砂岩是锑矿勘查的重点层位;隆林县弄桑-石家寨北西西—南东东向断裂带内隐伏岩体周边和西林县北西西—南东东向斗皇-西林断裂与北东—南西向断裂的交汇部位是锑矿勘查的有利区域。以上成果为研究区内锑金矿床成因和成矿规律认识提供新的思考,为区内锑矿床勘查提供方向。

Relationship between the formation, evolution of the ancient oil reservoir and metallogenesis

IN nature, there are many coexisting examples of petroleum with metallic ore deposit. There are metallicore deposits in the border and interior of many petroliferous basins, such as the bedded Pb-Zn ore depositin carbonate rock, gold sulfide ore deposit in black shale, cinnabar deposit, copper sandstone, kupferschiefer ore deposit, etc. (Tang Kuilian, 1995). The liquid hydrocarbon all was found in the Pb-Zn oredeposit, Mercury deposit, Carlin gold deposit (Shi Jixi et al., 1995) as well as the beds adjacentto them. There are a large number of bitumen and organic inclusions with hydrocarbon in the low-temperature Hg-Sb-Au ore concentrated district in southwestern margin to Yangtze platform. Fu Jiamao (1988)thought that they are remains after the ancient oil reservior destructed. In pace with constantly finding thecoexisting phenomena of metallic ore deposit and petroleum as well as further studying the relationship between both of them, it is progressively known that there are close links between oil/gas field and

云南锑(金)成矿带划分及有关成矿问题讨论

云南可划分11个锑(金)成矿带(区)。Sb-Au属同一成矿系列(Sb略晚),二者常相伴产出。滇东坡脚组(D1p)与滇西三合洞组(T3s),同为锑矿矿源层。滇东南与黔西区玄武岩喷溢早期的大厂层(P3d)、主期玄武岩组(P3β)、晚期龙潭组(P3l),三者含Sb、Au背景值远高于全球玄武岩,构成统一的Sb—Au矿源层(岩),在有利构造条件下,产出Sb矿(伴生Au)、Au矿(伴生Sb)或二者共存(广南堂上),其成因都与幔源玄武岩喷溢作用有关。