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1.
沉积盆地中金属成矿与油气成藏的耦合关系   总被引:10,自引:3,他引:7       下载免费PDF全文
沉积盆地中与油气密切相关的金属矿床主要包括密西西比河谷型(MVT)铅锌矿床、砂页岩型铜-铀矿床、黑色页岩中的金属硫化物矿床、沉积岩容矿的金-锑-砷-汞-铊矿床等。金属矿床与(古)油气藏在空间上的密切共生/伴生关系,暗示了二者成因上的有机联系。在许多MVT铅锌矿床和砂页岩型铜矿床中,与成矿关系密切的原油及其衍生物形成于矿化前,它们为随后的金属成矿直接提供还原硫或充当硫酸盐还原反应的还原剂。在另一些情况下,某些低温热液金属矿床,特别是Au、As、Hg、Sb、Tl矿床与油气表现出同源、同运、同聚的耦合关系,金属成矿与油气成藏同时或近同时进行。与油气具不同耦合关系的金属矿床常表现出不同的特点。与成藏和/或成矿有关的盆地流体大致可分为以碳氢化合物为主的有机流体、以含金属盐水溶液为主的无机流体以及同时富含烃类和金属组分的有机成矿流体3类,盆地中的成矿、成藏作用及其耦合关系受控于这三类流体的演化过程。沉积盆地中金属矿床与油气藏空间上密切的共生/伴生关系以及成矿、成藏过程和机理的相似性,使金属与油气矿产资源的协同勘探和综合预测成为可能。  相似文献   

2.
三塘湖盆地火山岩油气藏油气充注幕次及成藏年龄确定   总被引:2,自引:2,他引:0  
油气藏油气充注幕次和成藏年龄确定一直是成藏过程研究的热点和核心问题.通过60块流体包裹体系统分析,结合单井埋藏史投影方法,分析了三塘湖盆地火山岩油气藏的油气充注幕次和成藏期次,确定了其成藏年龄,从而对其油气成藏过程进行了研究,认为三塘湖盆地火山岩油气藏经历了石炭纪以来三期油气运聚的成藏过程.它们分别发生在259~230Ma、160~134Ma和70~0Ma,其中早期(海西印支期)油气成藏对盆地深部油气勘探具有重要意义.  相似文献   

3.
右江盆地是在杨子板块南缘早古生代基底之上发育起来的晚元古代-中生代沉积盆地,晚古生代以来盆地成矿-成藏流体的广泛活动,一方面形成了以微细浸染型金矿床为代表的一系列低温热液矿床,另一方面保留了众多的油气、油气苗和沥青显示[1-2].本文通过对若干具代表性的古油藏和金矿床流体包裹体的对比研究,探讨了右江盆地成矿-成藏流体的地球化学特征.  相似文献   

4.
通过对右江盆地二叠系生物礁古油藏流体包裹体的研究,探讨含油气流体的物理化学性质和油气演化程度。结果表明,含油气流体是一种多成分、多相态的不混溶体系,主要组分是有机质、CO2和H2O。成藏流体的温度变化于73~200℃,主要集中于90~160℃,与我国碳酸盐岩生油最佳温度或生油高峰温度一致。含油气流体的盐度低(多小于6%NaCl),密度中等(0.90~1.02 g/cm3),压力为4.2~65.4 MPa,有机组分中CH4占绝对优势,次为C2H6。从含油气流体的演化程度和物理化学特征来看,生物礁型油气藏应是右江盆地油气勘探的重点对象。  相似文献   

5.
华南中、低温成矿带主要由江南古陆的“江南型”金_锑矿带、湘黔汞矿带、西南卡林型金矿区和湘中锑矿带组成。其成矿时代有自东向西从燕山早期到中、晚期有变新的趋势; 矿种分布和成矿元素组合表现出对元古宇基底的继承性; 成矿流体的温度和盐度在大区域内从东到西和自南向北分别呈现降低和增高的趋势, 并且在古陆西、北侧的盆地中有盆地卤水混合的现象。研究表明, 华南中、低温成矿带的时空分布和成矿元素组合演化与华南燕山期花岗岩强烈活动的华南钨( 锡) 成矿域有密切的联系。这些大型矿集区都集中形成于燕山期, 并与川东南油气田一起, 共同构成了一个自南东向北西的高—中—低温热液矿床和油气矿藏的区域性矿化巨型分带。从而表现出大华南地区( 东南、中南和西南) 在燕山期曾经历过统一热场作用下的大范围流体运动和大规模成矿作用  相似文献   

6.
马东升 《矿床地质》1999,18(4):347-358
华南中、低温成矿带主要由江南古陆的"江南型"金-锑矿带、湘黔汞矿带、西南卡林型金矿区和湘中锑矿带组成.其成矿时代有自东向西从燕山早期到中、晚期有变新的趋势;矿种分布和成矿元素组合表现出对元古宇基底的继承性;成矿流体的温度和盐度在大区域内从东到西和自南向北分别呈现降低和增高的趋势,并且在古陆西、北侧的盆地中有盆地卤水混合的现象.研究表明,华南中、低温成矿带的时空分布和成矿元素组合演化与华南燕山期花岗岩强烈活动的华南钨(锡)成矿域有密切的联系.这些大型矿集区都集中形成于燕山期,并与川东南油气田一起,共同构成了一个自南东向北西的高-中-低温热液矿床和油气矿藏的区域性矿化巨型分带.从而表现出大华南地区(东南、中南和西南)在燕山期曾经历过统一热场作用下的大范围流体运动和大规模成矿作用.  相似文献   

7.
黑龙江省三矿沟矽卡岩型铁铜矿床流体包裹体研究   总被引:11,自引:2,他引:9  
刘军  武广  钟伟  朱明田 《岩石学报》2009,25(10):2631-2641
对黑龙江省三矿沟矽卡岩型铁铜矿床内花岗闪长岩中石英斑晶、硫化物阶段及石英-碳酸盐阶段的石英、方解石中流体包裹体的岩相学、显微测温学和显微激光拉曼光谱分析等的研究结果表明,流体包裹体有富液相、富气相和含子矿物多相包裹体3种类型;花岗闪长岩石英斑晶中的含子矿物多相包裹体均一温度均值为4320C,盐度在30.92 wt%~63.91 wt%NaCl eqv.之间,平均为52.96 wt%NaCl eqv.,代表了高温、高盐度岩浆流体;硫化物阶段形成的黄铜矿磁铁矿矿石中流体温度主要介于323~424℃之间,盐度介于8.95 wt%~62.51 wt%NaCl eqv.之间;硫化物阶段形成的黄铜矿矿石中流体温度主要介于333~441℃之间,盐度介于8.28 wt%~65.32 wt%NaCl eqv.之间;石英-碳酸盐阶段流体温度主要介于124~140℃之间,盐度介于1.65 wt%~4.34 wt%NaCl eqv.之间.铁铜矿石均形成于高温、高盐度阶段,以岩浆热液为主,在成矿晚期,由于大气降水的混合,形成了少量低温、低盐度流体,成矿流体以富Na、K、Ca、Cl-和CO~2_3-的高盐度流体为特征,主体属于NaCl-H_2O-CO_2-H_2S-CH_4体系.成矿流体在300~400℃区间内发生了强烈的沸腾作用,导致大量金属硫化物和少量金属氧化物沉淀,沸腾作用对三矿沟铁铜矿床的形成起到至关重要的作用.  相似文献   

8.
荷花坪锡多金属矿床是湘南地区新发现的一大型矿床, 主要由印支期矽卡岩型矿石和燕山期蚀变碎裂岩型矿石所组成, 且以前者为主体。本文在详细的野外调查和岩相学观察基础上, 将区内印支期成矿分为三个成矿阶段(I-含锡矽卡岩阶段; II-硫化物阶段; III-石英-方解石阶段), 燕山期成矿分为两个阶段(I-锡石-硫化物阶段; II-方解石阶段)。对不同期石英、绿柱石、方解石等矿物中流体包裹体的研究表明, 荷花坪矿床包裹体类型主要为H2O-NaCl型、H2O-NaCl-CO2型和少量纯CO2型。显微实验结果显示, 印支期成矿流体主要为低盐度(ω(NaCleq)=3%~10%)的H2O-NaCl和H2O-NaCl-CO2以及少量富CO2流体。三个成矿阶段的完全均一温度分别为290~390℃、190~260℃和140~180℃。成矿早阶段流体中含较多CO2, 晚阶段CO2含量减少, 主要为H2O-NaCl, 且Ca2+、Mg2+含量增高。燕山期成矿流体亦为低盐度(ω(NaCleq)=2%~10%)H2O-NaCl和H2O-NaCl-CO2, 二个成矿阶段的完全均一温度分别为190~340℃和130~170℃, 成矿早阶段流体中含较多CO2, 晚阶段CO2含量减少, 主要为NaCl-H2O。两期成矿从早到晚都呈现出盐度降低、密度增大的变化趋势。区内成矿流体主要来自岩浆和地下水热液, 成矿早阶段以岩浆流体为主, 晚阶段以地下水为主。区内锡成矿主要与含CO2的流体以及流体的沸腾作用有关, 铅锌矿化主要与盐-H2O溶液流体作用关系密切。  相似文献   

9.
中国西南部云南兰坪盆地因金顶Zn-Pn矿床和新发现的白秧坪超大型Cu-Co-Ag矿床而驰名。金顶矿床以白垩系和第三系陆相碎屑岩为主岩,拥有2亿吨矿石,平均品位Zn6.08%、Pb1.29%(1500万吨金属),是目前中国最大的Zn-Pb矿床,也是世界上形成时代最新且唯一产于陆相沉积岩容矿的超大型Zn-Pb矿床。不同于世界上人们公认的沉积岩容矿基本类型,即SST、MVT和Sedex型,金顶矿床也许代表了Zn-Pb矿床的一个新类型。通常认为兰坪盆地大规模成矿流体起源于盆地卤水,流体流动以重力驱动为主,压力体系接近静水压力。但基于矿田内水压破裂观察、流体包裹体研究和盆地流体动力学模拟,我们认为深部超压流体的注入对整个成矿系统起着重要作用。闪锌矿及相关脉石矿物(石英、天青石、方解石、石膏)中流体包裹体观测的均一温度主体在110~150℃,盐度(质量分数)在1.6%~18.0%NaCl;在时间上,大规模成矿主要阶段伴随着流体温度的不断升高和盐度的逐渐降低;在空间上,金顶矿区空间上从东到西,成矿流体温度明显降低,盐度系统性升高。富CO2流体包裹体揭示成矿流体曾高达(513~1364)×105Pa,大大高于静水压力。数值模拟表明,盆地沉积和压实产生的流体超压可以忽略,区域构造推覆也不足以产生如此高的流体压力。我们认为成矿流体超压很可能是幔源流体注入引起的;幔源含矿的相对高温低盐度流体沿导矿构造注入金顶穹隆构造-岩性圈闭并与其中富H2S的相对低温高盐度卤水混合是兰坪盆地大规模成矿的关键动力学过程。这个特殊的流体动力学过程和成矿系统,使兰坪盆地的成矿有别于世界其他沉积盆地已知的成矿作用。  相似文献   

10.
论盆地流体成矿/成烃作用的耦合关系   总被引:7,自引:1,他引:6  
沉积盆地中的油气聚集和某些金属矿床都是盆地演化过程中盆地流体活动的产物,是同一地质-构造格架内同一自然过程留下的物质表象。油气是被封存起来的、以碳氢化合物为主的盆地有机流体,而固态的金属矿石则大多是以水溶液相为主的盆地流体在适当的部位将所溶解携带的成矿金属组分沉淀卸载的结果。碳氢化合物源干沉积有机质的演化;成矿金属元素则可能是盆地流体从沉积物颗粒通过流-岩反应萃取来的。有机组分在成矿金属元素的活化萃取、迁移、直至沉淀就位的全过程中均起了非常重要的作用。在成岩压实作用阶段(相当干油气的初次析出阶段),油气与粘土水一道从生烃层内被挤出。从这个意义上讲,油气与部分成矿水溶液具有共同的起源。但在往后的运移和聚集就位过程中,由于水和油的物理化学特征不同,二发生了分离。从而造成了金属矿床与油气藏在空间上既相互依赖,又相互分离的复杂关系。  相似文献   

11.
The Youjiang basin, which flanks the southwest edge of the Yangtze craton in South China, contains many Carlin-type gold deposits and abundant paleo-oil reservoirs. The gold deposits and paleo-oil reservoirs are restricted to the same tectonic units, commonly at the basinal margins and within the intrabasinal isolated platforms and/or bioherms. The gold deposits are hosted by Permian to Triassic carbonate and siliciclastic rocks that typically contain high contents of organic carbon. Paragenetic relationships indicate that most of the deposits exhibit an early stage of barren quartz ± pyrite (stage I), a main stage of auriferous quartz + arsenian pyrite + arsenopyrite + marcasite (stage II), and a late stage of quartz + calcite + realgar ± orpiment ± native arsenic ± stibnite ± cinnabar ± dolomite (stage III). Bitumen in the gold deposits is commonly present as a migrated hydrocarbon product in mineralized host rocks, particularly close to high grade ores, but is absent in barren sedimentary rocks. Bitumen dispersed in the mineralized rocks is closely associated and/or intergrown with the main stage jasperoidal quartz, arsenian pyrite, and arsenopyrite. Bitumen occurring in hydrothermal veins and veinlets is paragenetically associated with stages II and III mineral assemblages. These observations suggest an intimate relationship between bitumen precipitation and gold mineralization. In the paleo-petroleum reservoirs that typically occur in Permian reef limestones, bitumen is most commonly observed in open spaces, either alone or associated with calcite. Where bitumen occurs with calcite, it is typically concentrated along pore/vein centers as well as along the wall of pores and fractures, indicating approximately coeval precipitation. In the gold deposits, aqueous fluid inclusions are dominant in the early stage barren quartz veins (stage I), with a homogenization temperature range typically of 230°C to 270°C and a salinity range of 2.6 to 7.2 wt% NaCl eq. Fluid inclusions in the main and late-stage quartz and calcite are dominated by aqueous inclusions as well as hydrocarbon- and CO2-rich inclusions. The presence of abundant hydrocarbon fluid inclusions in the gold deposits provides evidence that at least during main periods of the hydrothermal activity responsible for gold mineralization, the ore fluids consisted of an aqueous solution and an immiscible hydrocarbon phase. Aqueous inclusions in the main stage quartz associated with gold mineralization (stage II) typically have a homogenization temperature range of 200–230°C and a modal salinity around 5.3 wt% NaCl eq. Homogenization temperatures and salinities of aqueous inclusions in the late-stage drusy quartz and calcite (stage III) typically range from 120°C to 160°C and from 2.0 to 5.6 wt% NaCl eq., respectively. In the paleo-oil reservoirs, aqueous fluid inclusions with an average homogenization temperature of 80°C are dominant in early diagenetic calcite. Fluid inclusions in late diagenetic pore- and fissure-filling calcite associated with bitumen are dominated by liquid C2H6, vapor CH4, CH4–H2O, and aqueous inclusions, with a typical homogenization temperature range of 90°C to 180°C and a salinity range of 2–8 wt% NaCl eq. It is suggested that the hydrocarbons may have been trapped at relatively low temperatures, while the formation of gold deposits could have occurred under a wider and higher range of temperatures. The timing of gold mineralization in the Youjiang basin is still in dispute and a wide range of ages has been reported for individual deposits. Among the limited isotopic data, the Rb–Sr date of 206 ± 12 Ma for Au-bearing hydrothermal sericite at Jinya as well as the Re–Os date of 193 ± 13 Ma on auriferous arsenian pyrite and 40Ar/39Ar date of 194.6 ± 2 Ma on vein-filling sericite at Lannigou may provide the most reliable age constraints on gold mineralization. This age range is comparable with the estimated petroleum charging age range of 238–185 Ma and the Sm–Nd date of 182 ± 21 Ma for the pore- and fissure-filling calcite associated with bitumen at the Shitouzhai paleo-oil reservoir, corresponding to the late Indosinian to early Yanshanian orogenies in South China. The close association of Carlin-type gold deposits and paleo-oil reservoirs, the paragenetic coexistence of bitumens with ore-stage minerals, the presence of abundant hydrocarbons in the ore fluids, and the temporal coincidence of gold mineralization and hydrocarbon accumulation all support a coeval model in which the gold originated, migrated, and precipitated along with the hydrocarbons in an immiscible, gold- and hydrocarbon-bearing, basinal fluid system.  相似文献   

12.
为了探讨玄武岩铜矿成矿流体的特征,对滇黔交界地区峨眉山玄武岩铜矿3个成矿期次铜矿石中石英和方解石的气液包裹体进行了激光拉曼成分研究和均一温度、盐度测定,对古石油包裹体通过荧光显微镜进行了成分鉴定。结果表明:第1、2期次成矿流体主要为盆地卤水,其气液包裹体气液比小(一般5%~10%),w(NaCl)为8%~22%,气相为甲烷,液相为水,无子晶及液相CO2,均一温度为80℃~260℃;第2期次成矿流体除盆地卤水外,还有以古石油为代表的有机流体,古石油包裹体由液态烃、固体沥青和气相组成,均一温度变化大(30℃~290℃),液态烃以荧光性强的芳烃为主;第3期次成矿流体具有大气降水成因,其气液包裹体气液比一般为5%~10%,w(NaCl)〈4%,无子晶及液相CO2,均一温度140℃~270℃,但以小于200℃为主。从第1期次到第3期次,成矿流体盐度逐渐降低,特别是第3期次的盐度非常低,但温度变化不明显。本区最重要的自然铜沉淀富集成矿是第2期次不同性质成矿流体混合或成矿流体与有机流体混合、有机质的还原的结果。  相似文献   

13.
黔西南紫木凼金矿床流体包裹体特征及对成矿的指示意义   总被引:2,自引:0,他引:2  
紫木凼金矿床是黔西南微细浸染型(卡林型)金矿带上的一个代表性金矿床。本文对该矿床主成矿阶段(Ⅱ)石英和方解石以及晚成矿阶段(Ⅲ)方解石中的流体包裹体进行了岩相学和显微测温研究,结果表明,各成矿阶段包裹体类型有H2O包裹体、CO2包裹体、CO2-H2O包裹体、气相CH4包裹体和CH4-H2O包裹体5类,其中CO2包裹体和CO2-H2O包裹体只在主成矿阶段(Ⅱ)的石英中发育。主成矿阶段和晚阶段流体包裹体均一温度范围分别为180~220℃和100~180℃,盐度分别为0.35%~7.45% NaCl和0.18%~5.71% NaCl,密度分别变化于0.745~0.969 g/cm3和0.868~0.993 g/cm3,总体属于中低温、低盐度、中等密度的H2O-NaCl-CO2流体体系。矿床成矿过程是一个温度退缩、盐度降低、密度增大的过程。主成矿阶段H2O-NaCl-CO2流体发生不混溶作用,是导致矿质沉淀成矿的主要原因。CO2流体、CH4流体在金的成矿过程中起重要作用。  相似文献   

14.
This article presents the new mineralogical, fluid inclusion, and isotopic data for ores of the Novoshirokinsky base metal–gold deposit. Mineralogical sequence is supplemented and specified. The mineral assemblages containing native gold are studied. Morphology, grain size and chemical composition of native gold are described. Major parameters and composition of mineralizing fluids of the main ore stages at the deposit are estimated: main base metal (mid-temperature conditions, fluid salinity 3.1–13.1 wt % equiv NaCl) and carbonate–base metal (low-temperature conditions, fluid salinity 1.0–12.9 wt % equiv. NaCl). Sulfur isotopic composition of sulfides from commercial mineral assemblages has been studied. The δ34S value (+10.5 ± 1‰) of mineralizing fluid has been calculated. The Novoshirokinsky deposit is similar to epithermal deposits and is spatially related to the Late Jurassic porphyry system. Evidence is provided on carbonate rocks of basement involved in the ore-forming process.  相似文献   

15.
黔西南金矿成矿地质作用浅析   总被引:5,自引:3,他引:5  
对黔西南(包括部分桂西北)金矿床的地质、稳定同位素和流体包裹体等研究表明,黔西南微细浸染型金矿属燕山期Au—Sb—Hg—Tl—U—Mo—As—萤石成矿系列,该系列内的所有矿产地均位于扬子陆块与右江造山带交界线两侧,垭都—紫云和水城—盘县—罗平两条深大断裂夹持的地热异常区内。各矿床的硫同位素和均一温度、盐度、密度、压力、深度以及包裹体成份等,都自西北向东南发生系列性变化,成矿时代也有自西北向东南由老逐步变新的趋势。成矿流体各地不同,扬子陆块内金矿床主要为大气水沿断裂带深循环作用形成,右江造山带的金矿床是混有大气水的封存热卤水。  相似文献   

16.
造山型金矿是全球重要的金矿类型。造山型金矿包含三种类型:产于绿岩带的含金石英碳酸盐脉、产于浊积岩中的含金石英脉和产于条带状铁矿(BIF)中的含金石英脉。造山型金矿的形成受板块构造控制,处于压缩或者转换挤压的造山构造环境。造山型金矿中的绿岩带金矿主要受剪切带、转换断层控制,浊积岩型金矿受褶皱和层间走滑断层控制,而赋存于BIF中的金矿则受剪切带和断层所控制。在这些金矿床中发现了4类流体包裹体:H_2O-CO_2型、富CO_2型、气液包裹体和含Na Cl子矿物的包裹体。所有年代的造山型金矿成矿流体的成分均为低盐度的水溶液和富CO_2的流体,温度在200~400℃范围内。稳定同位素研究表明造山型金矿的成矿流体源自变质流体和岩浆流体。金在成矿流体中的络合物应为Au HS~-或Au H_2S。虽然成矿流体中有丰富的CO_2,但Au在CO_2流体中的溶解度很低,有丰富的CO_2时Au在H_2S中的溶解度增大。流体包裹体研究表明,Au的成矿流体是Na Cl-H_2O-CO_2体系的流体,并在成矿过程中发生了相分离,即Na Cl-H_2O-CO_2流体分成两个流体:H_2O-Na Cl和CO_2-H_2O,Au的沉淀是在这种相分离过程中发生的。  相似文献   

17.
The Huize Pb-Zn deposits of Yunnan Province, located in the south-central part of the Sichuan-Yunnan-Guizhou (SYG) Pb-Zn multimetal mineralization district (MMD), are strictly controlled by fault zones. The sources of ore-forming fluid in the deposits have been debated for a long time. Calcite, a gangue mineral, has uniform C and O isotopes. The δ13CPDB and δ18OSMOW values vary respectively from -2.1×10-3 to -3.5×10-3 (mean -2.8×10-3) and 16.7×10-3-18.6×10-3 (mean 17.7×10-3). No obvious difference can be found in C and O isotopes among occurrences and elevations and even ore-bodies. Types of inclusions include those of pure liquid (L), liquid-rich gas-liquid (L V), and three-phase ones containing a daughter mineral (S L V) and immiscible CO2 with three-phases (VCO2 LCO2 LH2O). Their homogenization temperatures vary from 110 to 400 ℃, and two peaks are shown. (87Sr/86Sr)0 ratios of calcite in the deposits are higher than those in the mantle and Emeishan basalts, and slightly higher than those in the Baizuo Formation, which the Huize lead-zinc deposits are found in. All of the (87Sr/86Sr)0 are low relative to those in the basement rocks. Fractionation of Sr isotope did not occur in the ore-forming fluid during the precipitation of minerals. The results indicate that the ore-forming fluid is homogeneous and derived from the mixing of different fluids. Gas-liquid inclusions can be separated into two groups in 300-400 ℃ with a salinity of 5 %-6 % and 12 %-16 % NaCl respectively. However, the salinities of inclusions vary from 7 % to 23 % NaCl in 100-300 ℃, especially in 150-250 ℃. The formation pressures of faulted zones are (50-320)×105 Pa. The estimated pressures of the overlying rocks on the ore bodies are 574×105-640×105 Pa. The pressures of ore-forming processes would be 145×105 to 754×105 Pa. Therefore, pressure sharply reduced and boiling occurred when the ore-forming fluid flew into the fault zones. As a result, the ore-forming fluid was highly concentrated, and metallic minerals began to precipitate from the fluid on a great scale. The high-grade lead-zinc deposits were formed when the fluid was under saturation or over-saturation conditions.  相似文献   

18.
在成矿地质背景和矿床地质特征研究基础上,对大金沟金矿主矿体中含矿石英脉流体包裹体开展了系统的岩相观察和显微测温工作。结果表明:大金沟金矿含矿石英脉中主要发育富液相的气液两相包裹体,偶见纯液相或气相包裹体。这些包裹体可分为低温高盐度(75℃~121℃,16.71 wt%NaCl~19.68 wt%NaCl)、低温低盐度(100℃~172℃,0.7 wt%NaCl~5.71 wt%NaCl)、中低温中低盐度(75℃~253℃,6.16 wt%NaCl~12.51 wt%NaCl)和高温中低盐度(331℃~420℃,4.96 wt%NaCl~12.51 wt%NaCl)等4类。大金沟金矿主成矿期流体包裹体的均一温度(75℃~253℃)和盐度(0.7 wt%NaCl~19.68 wt%NaCl)变化较大,且两者的相关性不明显,属典型的中低盐度流体体系,与造山过程相关的变质流体类似,表明该矿床可能为造山型金矿床。  相似文献   

19.
内蒙古额尔古纳市虎拉林金矿床成矿流体包裹体研究   总被引:2,自引:0,他引:2  
通过矿床流体包裹体岩相学、显微测温学和激光拉曼光谱成分分析,研究成矿流体性质,探讨了矿床成因类型.研究结果表明,流体包裹体以气液两相包裹体为主,少量含CO2三相、含子矿物三相和纯气相包裹体等.成矿流体均一温度为320~360℃,盐度为19.2%~21.8%,密度为0.73~0.90g/cm3,估算成矿压力为92.1~129.1MPa,成矿深度为3.07~4.3km.成矿流体气相成分以H2O为主,其次为CO2、CH4和N2,微量的C6H6、C2H6和C3H8等,总体属H2O-CO2-NaCl体系.成矿流体是一种不混溶流体,主要来源于深部岩浆,并可能有幔源组分参与.金主要是以金氯配合物的形式迁移.矿床的地质-地球化学特征与隐爆角砾岩型金矿类似,应属隐爆角砾岩型金矿床.  相似文献   

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