Fe同位素对藏南扎西康矿床成矿过程和成因的约束
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- 论文作者：王达 ; 孙祥 ; 郑有业
- 年：2015
- 作者机构：中国地质大学地质过程与矿产资源国家重点实验室;中国地质大学地质调查研究院;
- 会议召开时间：2015-10-18
- 会议录名称：中国地质学会同位素地质专业委员会成立三十周年暨同位素地质应用成果学术讨论会论文摘要集
- 语种：中文
- 分类号：P618.2
- 学会代码：DXHD
- 会议名称：中国地质学会同位素地质专业委员会成立三十周年暨同位素地质应用成果学术讨论会
- 会议地点：中国浙江宁波
- 主办单位：中国地质学会同位素地质专业委员会
- 学会名称：中国地质学会地质学报编辑部
- 页数：4
- 文件大小：1450k
- 原文格式：D
- 会议级别：全国
摘要
<正>扎西康锑多金属矿床位于北喜马拉雅锑金多金属成矿带,是该成矿带上目前发现的唯一的超大型矿床。关于其矿床成因存在诸多争论,有热泉成因(孟祥金等,2008)、地热卤水成因(张建芳等,2010)、岩浆热液成因(王艺云等,2012)和海底喷流沉积-改造成因(郑有业等,2012)。但是这些关于矿床成因理论的建立,大多基于C、H、O、S等同位分析,从成矿学的角度看,C、H、O、S等都是矿
引文
孟祥金,杨竹森,戚学祥,侯增谦,李振清.2008.藏南扎西康锑多金属矿硅-氧-氢同位素组成及其对成矿构造控制的响应.岩石学报,24(7):1649~1655.
王艺云,唐菊兴,郑文宝,林彬,冷秋锋,陈伟.2012.西藏隆子县扎西康锌多金属矿床矿石组构研究及成因探讨.地球学报,33(4):681~692.
张刚阳,郑有业,张建芳,张苏坤,樊子晖.2011.西藏沙拉岗锑矿控矿构造及成矿时代约束.岩石学报,27(7):2143~2149.
张建芳,郑有业,张刚阳,高顺宝,叶先仁,张众等.2010.北喜马拉雅扎西康铅锌锑银矿床成因的多元同位素制约.地球科学:中国地质大学学报,35:1000~1010.
郑有业,刘敏院,孙祥,原恩会,田立明,郑海涛,张刚阳,张立华.2012.西藏扎西康锑多金属矿床类型、发现过程及意义.地球科学:中国地质大学学报,37(5):1003~1014.
Beard B L,Johnson C M.1999.High precision iron isotope measurements of terrestrial and lunar materials.Geochimica Et Cosmochimica Acta,63(11):1653~1660.
Beard B L,Johnson C M,Von Damm K L,Poulson R L.2003.Iron isotope constraints on fe cycling and mass balance in oxygenated earth oceans.Geology,31(7):629~632.
Butler I B,Archer C,Vance D,Oldroyd A,Rickard D.2005.Fe isotope fractionation on Fe S formation in ambient aqueous solution.Earth and Planetary Science Letters,236(1):430~442.
He Y,Ke S,Teng F,Wang T,Wu H,Lu Y,Li S.2015.High‐precision iron isotope analysis of geological reference materials by high‐resolution mc‐icp‐ms.Geostandards&Geoanalytical Research,39:341~356.
Johnson C M,Skulan J L,Beard B L,Sun H,Nealson K H,Braterman P S.2002.Isotopic fractionation between Fe(III)and Fe(II)in aqueous solutions.Earth and Planetary Science Letters,195(1):141~153.
Markl G,Von Blanckenburg F,Wagner T.2006.Iron isotope fractionation during hydrothermal ore deposition and alteration.Geochimica Et Cosmochimica Acta,70(15):3011~3030.
Richter F M,Dauphas N,Teng F Z.2009.Non-traditional fractionation of non-traditional isotopes:evaporation,chemical diffusion and Soret diffusion.Chemical Geology,258(1):92~103.
Rouxel O,Fouque,Y,Ludden J N.2004.Subsurface processes at the lucky strike hydrothermal field,mid-atlantic ridge:evidence from sulfur,selenium,and iron isotopes 1 1 associate editor:s.sheppard.Geochimica Et Cosmochimica Acta,68(68):2295~2311.
Rouxel O,Iii W C.S,Bach W,Edwards K J.2008.Integrated fe-and s-isotope study of seafloor hydrothermal vents at east pacific rise9-10°n.Chemical Geology,252:214~227.
Sun J,Zhu X,Chen Y,Fang N.2013.Iron isotopic constraints on the genesis of Bayan Obo ore deposit,Inner Mongolia,China.Precambrian Research,235:88~106.
Wang Y,Zhu X K,Mao J W,Li Z H,Cheng Y B.2011.Iron isotope fractionation during skarn-type metallogeny:a case study of Xinqiao Cu-S-Fe-Au deposit in the Middle-Lower Yangtze valley.Ore Geology Reviews,43(1):194~202.
王艺云,唐菊兴,郑文宝,林彬,冷秋锋,陈伟.2012.西藏隆子县扎西康锌多金属矿床矿石组构研究及成因探讨.地球学报,33(4):681~692.
张刚阳,郑有业,张建芳,张苏坤,樊子晖.2011.西藏沙拉岗锑矿控矿构造及成矿时代约束.岩石学报,27(7):2143~2149.
张建芳,郑有业,张刚阳,高顺宝,叶先仁,张众等.2010.北喜马拉雅扎西康铅锌锑银矿床成因的多元同位素制约.地球科学:中国地质大学学报,35:1000~1010.
郑有业,刘敏院,孙祥,原恩会,田立明,郑海涛,张刚阳,张立华.2012.西藏扎西康锑多金属矿床类型、发现过程及意义.地球科学:中国地质大学学报,37(5):1003~1014.
Beard B L,Johnson C M.1999.High precision iron isotope measurements of terrestrial and lunar materials.Geochimica Et Cosmochimica Acta,63(11):1653~1660.
Beard B L,Johnson C M,Von Damm K L,Poulson R L.2003.Iron isotope constraints on fe cycling and mass balance in oxygenated earth oceans.Geology,31(7):629~632.
Butler I B,Archer C,Vance D,Oldroyd A,Rickard D.2005.Fe isotope fractionation on Fe S formation in ambient aqueous solution.Earth and Planetary Science Letters,236(1):430~442.
He Y,Ke S,Teng F,Wang T,Wu H,Lu Y,Li S.2015.High‐precision iron isotope analysis of geological reference materials by high‐resolution mc‐icp‐ms.Geostandards&Geoanalytical Research,39:341~356.
Johnson C M,Skulan J L,Beard B L,Sun H,Nealson K H,Braterman P S.2002.Isotopic fractionation between Fe(III)and Fe(II)in aqueous solutions.Earth and Planetary Science Letters,195(1):141~153.
Markl G,Von Blanckenburg F,Wagner T.2006.Iron isotope fractionation during hydrothermal ore deposition and alteration.Geochimica Et Cosmochimica Acta,70(15):3011~3030.
Richter F M,Dauphas N,Teng F Z.2009.Non-traditional fractionation of non-traditional isotopes:evaporation,chemical diffusion and Soret diffusion.Chemical Geology,258(1):92~103.
Rouxel O,Fouque,Y,Ludden J N.2004.Subsurface processes at the lucky strike hydrothermal field,mid-atlantic ridge:evidence from sulfur,selenium,and iron isotopes 1 1 associate editor:s.sheppard.Geochimica Et Cosmochimica Acta,68(68):2295~2311.
Rouxel O,Iii W C.S,Bach W,Edwards K J.2008.Integrated fe-and s-isotope study of seafloor hydrothermal vents at east pacific rise9-10°n.Chemical Geology,252:214~227.
Sun J,Zhu X,Chen Y,Fang N.2013.Iron isotopic constraints on the genesis of Bayan Obo ore deposit,Inner Mongolia,China.Precambrian Research,235:88~106.
Wang Y,Zhu X K,Mao J W,Li Z H,Cheng Y B.2011.Iron isotope fractionation during skarn-type metallogeny:a case study of Xinqiao Cu-S-Fe-Au deposit in the Middle-Lower Yangtze valley.Ore Geology Reviews,43(1):194~202.