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Re-Os Age of Cu-Ni Ores from the Huangshandong Cu-Ni Sulfide Deposit in the East Tianshan Mountains and Its Implication for Geodynamic Processes 被引量:28
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作者 MAOJingwen YANGJianmin +3 位作者 QUWenjun DUAndao WANGZhiliang HANChunming 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2003年第2期220-226,共7页
An isochron age of 282±20 (95% conf. limit) Ma of the sulfide ores in the Huangshandong Cu-Ni sulfide deposit, the East Tianshan Mountains has been obtained through Re-Os isotopic measurement. The age implies tha... An isochron age of 282±20 (95% conf. limit) Ma of the sulfide ores in the Huangshandong Cu-Ni sulfide deposit, the East Tianshan Mountains has been obtained through Re-Os isotopic measurement. The age implies that the Cu-Ni sulfide deposit and other related deposits in the same area occurred in a Permian extensional environment of post-collision instead of Devonian-Early Carboniferous ophiolite-related oceanic or island arc environments inferred before. It shares the same ages with the orogenic and epithermal gold deposit systems in the same area. An initial 187Os/188Os ratio of 0.25±0.04 (1σ) and a γos value of 99 on average display the participation of large quantities of crustal components into the rock-forming and ore-forming system during mineralization and magmatic emplacement. 展开更多
关键词 Huangshandong cu-ni sulfide deposit East Tianshan mountains PERMIAN Re-Os age
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REE Characteristics of the Kalatongke Cu-Ni Deposit, Xinjiang, China 被引量:9
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作者 WANGYuwang WANGJingbin +2 位作者 WANGLijuan WANGYong TUCaineng 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2004年第2期396-403,共8页
On the basis of the study on the REE geochemistry of the ore minerals and host rocks of the Kalatongke Cu-Ni deposit, Xinjiang, it is indicated that the major ore minerals, sulfides, were sourced from the host mafic-u... On the basis of the study on the REE geochemistry of the ore minerals and host rocks of the Kalatongke Cu-Ni deposit, Xinjiang, it is indicated that the major ore minerals, sulfides, were sourced from the host mafic-ultramafic magma. Characterized by low REE content of sulfide, such a Cu-Ni sulfide deposit occurring in the orogen is obviously different from that on the margin of the craton. Because the mafic-ultramafic rocks from the Cu-Ni sulfide deposit occurring in the orogen is water-rich and the REEs of some sulfides show a particular 'multiple-bending' pattern, which suggests coexistence of multiple liquid phases (fluid and melt), the sulfide melt possibly contains a great deal of hydrothermal fluids and increasingly developed gases and liquid-rich ore-forming fluids after the main metallogenic epoch (magmatic segregation stage). 展开更多
关键词 cu-ni sulfide deposit rare earth elements water-rich mafic-ultramafic rock XINJIANG
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Geochemistry of Ore-bearing Lamprophyre from the Cu-Ni Deposit in Dhi Samir,Yemen 被引量:2
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作者 ZUO Liyan PEI Rongfu +3 位作者 SHUAI Kaiye YANG Fengqi ZHU Riwei ZHANG Liemeng 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2011年第1期200-210,共11页
Magmatic Cu-Ni sulfide deposits are generally associated with mafic-ultramafic rocks and it has not been reported that lamprophyre is one of the surrounding rocks of Cu-Ni sulfide deposits.The Dhi Samir deposit in Yem... Magmatic Cu-Ni sulfide deposits are generally associated with mafic-ultramafic rocks and it has not been reported that lamprophyre is one of the surrounding rocks of Cu-Ni sulfide deposits.The Dhi Samir deposit in Yemen,however,is a rare example of Cu-Ni deposits which are hosted in lamprophyre dikes.In this paper,comprehensive research is made on petrology,petrochemistry and isotope geochemistry for Cu-Ni-bearing rocks in the Dhi Samir area and the results show that dark rocks related to Cu-Ni orebodies are sodium-weak potassium and belong to calc-alkaline series lamprophyre,especially camptonite,characterized by enriched alkali,iron and titanium.In these rocks large-ion-lithophile elements are obviously concentrated,while high field strength elements slightly depleted,showing clear negative anomalies of Ta and Nb,and weak deficiency of Ti.TheΣREE is very high(225.67-290.05 ppm) and the REE partition curves are flat and right-inclined,featuring a LREE-enriched pattern with low negative Eu anomalies.Study of magmatic source areas indicates that the rocks have low(87Sr/86Sr) and highεNd(t),and the magmas were probably derived from the enriched mantle I(EM-I) end-member.Based on the LA-ICPMS on zircon U-Pb isotope dating,the lamprophyre in the Dhi Samir mining area has an age of 602±2.6 Ma,indicating that the rock was formed in the late Proterozoic and in an intraplate setting due to magmatism of an extensional environment in the post-Pan-Africa orogeny. 展开更多
关键词 LAMPROPHYRE geochemical characteristics cu-ni deposit in Dhi Samir Yemen
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First Report of Zircon U-Pb Ages from Lubei Cu-Ni Sulfide Deposit in East Tianshan of Central Asian Orogenic Belt, NW China 被引量:3
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作者 LI Ping ZHAO Tongyang +2 位作者 ZHU Zhixin TIAN Jiangtao LI Dahai 《Acta Geologica Sinica(English Edition)》 CAS CSCD 2018年第2期855-856,共2页
Objective The East Tianshan mafic-ultramafic rocks belt mainly produced in the eastern Jueluotage belt is an important part of the Central Asia Orogenic Belt (CAOB). The well- known deposits including Huangshan, Hu... Objective The East Tianshan mafic-ultramafic rocks belt mainly produced in the eastern Jueluotage belt is an important part of the Central Asia Orogenic Belt (CAOB). The well- known deposits including Huangshan, Huangshandong, Tulaergen, Hulu, Xiangshan were have been consecutively discovered in this belt (Duan Xingxing et al., 2016). The new discovery of the Lubei Cu-Ni sulfide deposit in recent years, which locates in the west of Jueluotage belt, has great significance to the westward extension of the East Tianshan Cu-Ni metallogenic belt. To determine whether the mineralization age of the Lubei Cu-Ni sulfide deposit is consistent with other typical deposits, this study conducted zircon U-Pb geochronology on the diorite from the Lubei Cu-Ni sulfide deposit in order to provide new information for further exploring direction of Cu-Ni prospecting in East Tianshan. 展开更多
关键词 PB First Report of Zircon U-Pb Ages from Lubei cu-ni Sulfide deposit in East Tianshan of Central Asian Orogenic Belt NW China Cu NI
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Rhenium-Osmium Isotope Constraints on the Origin of the Tianyu Cu-Ni Deposit in the East Tianshan Orogenic Belt, Xinjiang, NW China
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作者 HAN Chunming XIAO Wenjiao +5 位作者 AO Songjian ZHANG Jien SONG Dongfang ZHANG Zhiyong SONG Shuaihua XIE Mingcai 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2022年第2期525-535,共11页
The Tianyu Cu-Ni sulfide deposit occurs in the north margin of the Central Tianshan Arc in East Tianshan orogenic belt, Xinjiang, NW China. The intrusions consist of gabbro, peridotite, and olivine pyroxenite. The per... The Tianyu Cu-Ni sulfide deposit occurs in the north margin of the Central Tianshan Arc in East Tianshan orogenic belt, Xinjiang, NW China. The intrusions consist of gabbro, peridotite, and olivine pyroxenite. The peridotite and pyroxenite are the main host rock for the Cu-Ni ores. Rhenium and osmium isotopic analyses of Ni-and Cu-bearing sulfide minerals from the deposit have been used to determine the source of osmium, and by inference, the sources of ore metals. Sulfide ore samples have Os and Re concentrations varying in the ranges 1.85 to 4.58 ppb and 93.56 to 146.00 ppb, respectively. An initial ^(187)Os/^(188)Os ratio ranges from 0.86 to 1.23 for the ores and the γOs values from 592 to 2227. Osmium isotopic data suggest that the Tianyu intrusion and associated Cu-Ni mineralization has derived from crustal-contaminated mantle melts. The intrusions early show island-arc geochemical signatures, which indicate that the Hulu mafic–ultramafic intrusions, along with the Cu-Ni deposit, formed as a result of subduction of oceanic crust in the Early Permian. 展开更多
关键词 rhenium-osmium isotope cu-ni deposit Tianyu intrusion East Tianshan orogenic belt XINJIANG
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GENESIS AND ORE-FORMING PATTERN OF THE PARTICULARLY LARGE LANCHANG MULTIMETAL DEPOSIT IN LANCHANG,YUNNAN, CHINA
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《Geotectonica et Metallogenia》 1994年第Z2期74-75,共2页
关键词 ORE Pb CHINA GENESIS AND ORE-FORMING PATTERN OF THE PARTICULARLY LARGE LANCHANG multimetal deposit IN LANCHANG YUNNAN
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Geochemical Characteristics,Genesis of Concealed Cu-rich Ore Body in the Jinchuan Deposit,Northwestern China,and Its Prospecting 被引量:9
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作者 GAO Yalin TANG Zhongli +2 位作者 ZHANG Mingjie TIAN Yulong XIAO Lizhong 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2009年第6期1085-1100,共16页
The Jinchuan deposit is hosted by the olivine-rich ultramafic rock body, which is the thirdlargest magmatic sulfide Ni-Cu deposit in the world currently being exploited. Seeking new relaying resources in the deep and ... The Jinchuan deposit is hosted by the olivine-rich ultramafic rock body, which is the thirdlargest magmatic sulfide Ni-Cu deposit in the world currently being exploited. Seeking new relaying resources in the deep and the border of the deposit becomes more and more important. The ore body, ore and geochemistry characteristics of the concealed Cu-rich ore body are researched. Through spatial analysis and comparison with the neighboring II1 main ore body, the mineralization rule of the concealed Cu-rich ore body is summed up. It is also implied that Cu-rich magma may exist between Nirich magma and ore pulp during liquation differentiation in deep-stage chambers, which derives from deep-mantle Hi-MgO basalt magma. It is concluded that the type of ore body has features of both magmatic liquation and late reconstruction action. It has experienced three stages: deep liquation and pulsatory injection of the Cu- and PPGE-rich magma, concentration of tectonic activation, and the later magma hydrothermal superimposition. In addition, the Pb and S isotopes indicate the magma of I6 concealed Cu-rich ore body originates predominantly from mantle; however, it is interfused by minute crust material. Finally, it is inferred that the genesis of the Cu-Ni sulfide deposit is complex and diverse, and the prospect of seeking new deep ore bodies within similar deposits is promising, especially Cu-rich ore bodies. 展开更多
关键词 cu-ni sulfide deposit Cu-rich magma Cu-rich ore body PROSPECTING Jinchuan
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华北地台北缘中段银多金属矿床与火山岩 被引量:8
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作者 肖成东 艾永富 《地质论评》 CAS CSCD 北大核心 1999年第S1期488-494,共7页
该区的银多金属矿床在空间上受前中生代基底东西向深大断裂和中生代的北东向构造岩浆带控制,由东向西构成北东—东西向带状分布的银多金属矿带集中区。其成矿与中元古代和中生代火山活动关系密切;即中元古代大红峪碱性玄武岩,中生代的... 该区的银多金属矿床在空间上受前中生代基底东西向深大断裂和中生代的北东向构造岩浆带控制,由东向西构成北东—东西向带状分布的银多金属矿带集中区。其成矿与中元古代和中生代火山活动关系密切;即中元古代大红峪碱性玄武岩,中生代的酸性偏碱性火山岩。古元古代的变粒岩、中、新元古代的沉积岩中的特定层位和中生代燕山期张家口旋回火山岩具有矿源层特征。根据地质地球化学特征,提出该区存在四类银多金属矿床的认识。 展开更多
关键词 华北地台北缘 火山岩 矿源层 银多金属矿床
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湖南黄沙坪铅锌矿多金属矿床构造控矿特征及成矿浅析 被引量:24
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作者 李石锦 《大地构造与成矿学》 EI CAS CSCD 1997年第4期339-346,共8页
根据黄沙坪铅锌矿床形成地质背景,成矿地质特点,矿床地球化学特征。该矿床是以包括花岗质岩浆作用在内的多种成矿作用共同控制再造富集型的多因复成矿床。区内的燕山期花岗斑岩、花斑岩侵入体的内外接触带的接触构造和南北向各迭加断... 根据黄沙坪铅锌矿床形成地质背景,成矿地质特点,矿床地球化学特征。该矿床是以包括花岗质岩浆作用在内的多种成矿作用共同控制再造富集型的多因复成矿床。区内的燕山期花岗斑岩、花斑岩侵入体的内外接触带的接触构造和南北向各迭加断裂与铅锌矿化关系最为密切。 展开更多
关键词 铅锌矿床 多金属矿床 控矿构造 矿床成矿
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思茅大平掌铜多金属矿床地质特征及成矿机制 被引量:7
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作者 杨贵来 胡光道 《云南地质》 2001年第4期347-360,共14页
大平掌铜矿属火山成因铜多金属矿床。主矿体———浸染状矿体为次火山热液型 ,受英安岩等组成的火山穹窿构造及隐爆角砾岩筒构造所控制 ,赋存部位为火山管道之隐爆角砾 次火山岩相 ;块状矿体是在D2 ~C1海相火山喷发时期形成 ,受后期... 大平掌铜矿属火山成因铜多金属矿床。主矿体———浸染状矿体为次火山热液型 ,受英安岩等组成的火山穹窿构造及隐爆角砾岩筒构造所控制 ,赋存部位为火山管道之隐爆角砾 次火山岩相 ;块状矿体是在D2 ~C1海相火山喷发时期形成 ,受后期构造及火山 次火山岩体侵位破坏 ,呈角砾状分布在构造破碎带中。 展开更多
关键词 铜多金属矿床 细碧角斑岩 次火山热液喷流沉积 大平掌 思茅 成矿机制
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索尔库都克-哈腊苏铜钼金多金属矿集区成矿规律 被引量:4
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作者 王睿 游军 +1 位作者 丁汝福 宋慈安 《云南地质》 2011年第3期381-385,328,共6页
总结矿集区不同矿种、不同成因类型矿床的基本特征,研究矿床成矿规律,认为成矿集中在海西期,矿床形成先后顺序从早到晚为依次为:乔夏哈拉铁铜金矿、哈腊苏铜金(钼)矿、希勒库都克铜钼矿、沙尔布拉克金矿、喀拉通克铜镍矿、索尔库都克铜... 总结矿集区不同矿种、不同成因类型矿床的基本特征,研究矿床成矿规律,认为成矿集中在海西期,矿床形成先后顺序从早到晚为依次为:乔夏哈拉铁铜金矿、哈腊苏铜金(钼)矿、希勒库都克铜钼矿、沙尔布拉克金矿、喀拉通克铜镍矿、索尔库都克铜钼矿。且具有成带分布、分段集中,地层、构造、岩体控矿,张裂成矿的特点。 展开更多
关键词 多金属矿 矿集区 多因素控矿 成带多段 新疆阿尔泰东段
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大瑶山北侧铜多金属矿成矿及构造地球化学找矿 被引量:6
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作者 张雪亮 吴荣华 +1 位作者 赵延朋 赵俊宏 《云南地质》 2013年第1期56-59,共4页
北东向深大断裂成矿前生成,控制岩浆岩侵入及成矿带展布,多期次构造、岩浆活动,提供成矿物质及其活化热源。矿床具典型的水平垂向分布规律。应用构造地球化学方法找矿效果显著。
关键词 铜多金属矿 南北中各不相同 构造控矿 成矿规律明显 桂东大瑶山北侧
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金平平安寨金多金属矿成矿规律及找矿前景 被引量:2
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作者 舒培华 杨昌毕 李玉光 《云南地质》 2012年第2期166-170,152,共6页
受基性、中碱性岩体控制,多金属矿均产于喜马拉雅期碱性正长岩带岩体与断裂交汇的复合部位,矿化与构造关系密切,且以Cu-Mo为中心,向Pb-Zn-金过渡。找矿靶区可分为高、中、低温三类。
关键词 金铜钼多金属矿 碱性正长岩带 断裂岩体交汇部 喜马拉雅期 云南金平平安寨
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香格里拉欠虽铜铁矿床地质特征及成矿预测 被引量:4
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作者 孙贵荣 董建春 《云南地质》 2009年第3期263-267,共5页
矿床成因与地层、构造、岩浆岩关系密切,根据矿床分布规律和找矿标志、控矿因素,可进行有效的成矿预测,为进一步勘查提供有利依据。
关键词 铜铁多金属矿 种成矿类型 高精度磁测异常 找矿前景 云南香格里拉
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山西代县滩上一带金、多金属矿矿床特征及矿床成因浅析 被引量:4
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作者 杨全林 《科技创新与生产力》 2011年第3期100-102,共3页
介绍了山西省忻州市代县滩上一带区域地质背景和矿区地质概况,描述了该区的矿床产出特征,分析了该区的成矿控制因素和矿床成因,提出了该区是寻找次火山—岩浆热液型金、多金属矿的有利地段的结论。
关键词 代县 多金属 矿床特征 矿床成因
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香格里拉陆家村银金多金属矿矿化特征及找矿标志 被引量:1
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作者 黄琴辉 《云南地质》 2010年第4期499-502,共4页
研究区浅部以断裂破碎带控制的热液脉型Cu、Au、Pb、Ag矿床为主,深部形成斑岩型Cu、Mo矿床。矿体受地层及断裂构造双重控制。硅化、黄(褐)铁矿化与矿化关系最为密切,是主要的围岩蚀变,亦为主要的找矿标志。
关键词 银金多金属矿床 热液脉型 成矿地质特征 找矿标志 香格里拉陆家村
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云南泸水雪蒙山铜镍多金属矿成因探讨
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作者 黄发梅 刘振兴 苏泰民 《云南地质》 2013年第2期244-246,共3页
矿体赋存于石炭系/泥盆系侵入辉长辉绿岩互层带中。铜镍成矿物质大部分源于地幔,由基性、超基性岩浆带至地壳上部,岩体既是铜镍硫化物的母岩,又是矿体的直接围岩,属熔离—结晶分异、矿浆依次贯入叠加型矿床。
关键词 铜镍多金属矿床 岩浆熔离型 深大断裂控制 产出部位稳定 云南泸水雪蒙山
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激电中梯测量工作在多金属找矿中的应用 被引量:34
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作者 崔东郓 王伟建 《贵州地质》 2009年第3期218-220,共3页
该项目在全面收集、分析研究前人资料的基础上,根据以往区域化探工作所圈定出的金异常和Cu、Pb、Zn多金属异常区,作为进一步找矿的靶区,根据金与硫化物关系极为密切的特点,采用了地球物理勘探电法中激发极化法,终于在测区发现了一条较... 该项目在全面收集、分析研究前人资料的基础上,根据以往区域化探工作所圈定出的金异常和Cu、Pb、Zn多金属异常区,作为进一步找矿的靶区,根据金与硫化物关系极为密切的特点,采用了地球物理勘探电法中激发极化法,终于在测区发现了一条较为明显的近南北向激电异常带,反应了埋藏的极化体的存在,同时结合该区区域化探异常成果认为,该激电异常将是寻找金矿的有利地段。激发激化法物探测量工作方法的成功使用,为该区后续地质勘探工作进一步缩小了找矿靶区,预示了埋藏的金或多金属矿化体的存在。 展开更多
关键词 激电中梯 隐伏矿体 金多金属矿 新疆
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物化探在保山核桃坪矿床中的综合应用 被引量:5
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作者 杨孝武 官德任 《云南地质》 2011年第1期78-82,共5页
核桃坪铅锌铜多金属矿的靶区选择、评价及矿床发现中,由浅入深的物化探工作,在8个综合物化探异常区都找到多金属硫化物矿体,金厂河矿区实现隐伏深部找矿的重大突破。并总结出了一套合理的找矿勘查技术。
关键词 铅锌铜多金属矿 物化探方法 隐伏矿突破 综合应用效果 云南保山核桃坪
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云南绿春地区金多金属矿成矿背景及找矿方向 被引量:1
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作者 徐荣 张保龙 +2 位作者 李高良 康金勇 师娅芳 《云南地质》 2012年第4期434-437,共4页
金多金属矿主要赋存于志留系变质岩、二叠系火山岩及第三系碎屑岩中,小型脆韧性断裂破碎带、接触蚀变矿化带、地球化学异常是赋矿找矿前提。
关键词 金多金属矿 脆韧性剪切构造 陆缘弧带 找矿方向 云南绿春
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