【引用本文】 李宁, 杨富全, 李超, 等. 新疆东天山小白石头钨(钼)矿辉钼矿Re-Os同位素年龄及成矿时代[J]. 岩矿测试, 2019, 38(1): 112-122. doi: 10.15898/j.cnki.11-2131/td.201805250064
LI Ning , YANG Fu-quan , LI Chao , et al. Re-Os Isotopic Age of Molybdenite from the Xiaobaishi W-(Mo) Deposit, Eastern Tianshan, Xinjiang and Its Geological Implication[J]. Rock and Mineral Analysis, 2019, 38(1): 112-122. doi: 10.15898/j.cnki.11-2131/td.201805250064

新疆东天山小白石头钨(钼)矿辉钼矿Re-Os同位素年龄及成矿时代

1. 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室, 北京 100037;

2. 国家地质实验测试中心, 北京 100037;

3. 中国科学院新疆生态与地理研究所, 新疆矿产资源研究中心, 新疆 乌鲁木齐 830011

收稿日期: 2018-05-25  修回日期: 2018-07-23 

基金项目: 国家自然科学基金项目(41672072)

作者简介: 李宁,博士研究生,主要从事矿床学研究。E-mail:512359151@qq.com。。

Re-Os Isotopic Age of Molybdenite from the Xiaobaishi W-(Mo) Deposit, Eastern Tianshan, Xinjiang and Its Geological Implication

1. Institute of Mineral Resources, Chinese Academy of Geological Sciences;Key Laboratory of Metallogeny and Mineral Assessment, Ministry of National Resources, Beijing 100037, China;

2. National Research Center for Geoanalysis, Beijing 100037, China;

3. Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences;Xinjiang Research Center for Mineral Resources, Urumqi 830011, China

Received Date: 2018-05-25
Revised Date: 2018-07-23

摘要:小白石头钨(钼)矿床位于新疆东天山造山带中的中天山地块南缘,该矿床是一个由黑云母花岗岩和花岗闪长岩侵入中元古界卡瓦布拉格群形成的矽卡岩型钨(钼)矿床。辉钼矿作为其主要的矿石矿物之一,呈不同产出状态分布于花岗闪长岩、黑云母花岗岩、矽卡岩和石英脉中。目前,对于小白石头钨(钼)矿成矿时代尚有争议,特别是与花岗闪长岩有关的辉钼矿化形成时代缺乏精确的限定。本文选取与花岗闪长岩有关的不同产状辉钼矿进行Re-Os同位素定年,获得Re-Os加权平均模式年龄为245.0±1.7Ma,Re-Os等时线年龄为245.5±4.3Ma。准确的Re-Os同位素定年限定小白石头钨(钼)矿床的成矿年龄和花岗闪长岩的侵位年龄为245Ma左右,为矿床模型建立和找矿方向确定提供了关键依据,同时也为东天山区域成矿规律总结提供了重要的年代学证据,并指出新疆东天山-甘肃北山地区存在一条找矿潜力巨大的三叠纪钨钼成矿带。

关键词: 东天山, 小白石头钨(钼)矿床, 辉钼矿, Re-Os同位素年龄, 花岗闪长岩, 三叠纪

Re-Os Isotopic Age of Molybdenite from the Xiaobaishi W-(Mo) Deposit, Eastern Tianshan, Xinjiang and Its Geological Implication

KEY WORDS: East Tianshan, Xiaobaishitou W-(Mo) deposit, molybdenite, Re-Os isotopic age, granodiorite, Triassic

本文参考文献

[1]

杨富全,秦纪华,刘锋,等.新疆准噶尔北缘玉勒肯哈腊苏铜(钼)矿区韧性剪切变形时代——来自白云母和黑云母Ar-Ar年龄的约束[J].大地构造与成矿学,2013,37(1):1-10.

Yang F Q,Qin J H,Liu F,et al.Ar-Ar dating of the ductile shear zones in the Yulekenhalasu Cu-(Mo) ore deposit[J].Geotectonica et Metallogenia,2013,37(1):1-10.

[2]

Yang F Q,Liu F,Li Q,et al.In situ LA-MC-ICP-MS U-Pb geochronology of igneous rocks in the Ashele Basin,Altay orogenic belt,Northwest China:Constraints on the timing of polymetallic copper mineralization[J].Journal of Asian Earth Sciences,2014,79:477-496.

[3]

朱乔乔,谢桂青,蒋宗胜,等.湖北金山店大型矽卡岩型铁矿热液榍石特征和原位微区LA-ICP-MS U-Pb定年[J].岩石学报,2014,30(5):1322-1338.

Zhu Q Q,Xie G Q,Jiang Z S,et al.Characteristics and in situ U-Pb dating of hydrothermal titanite by LA-ICP-MS of the Jingshandian iron skarn deposit,Hubei Province[J].Acta Petrologica Sinica,2014,30(5):1322-1338.

[4]

洪为,张作衡,李华芹,等.新疆西天山查岗诺尔铁矿床成矿时代——来自石榴石Sm-Nd等时线年龄的信息[J].矿床地质,2012,31(5):1067-1074.

Hong W,Zhang Z H,Li H Q,et al.Metal logenic epoch of Chagangnuoer iron deposit in Western Tianshan Mountains,Xinjiang:Information from garnet Sm-Nd isochron age[J].Mineral Deposits,2012,31(5):1067-1074.

[5]

Liu L J,Zhou T F,Zhang D Y,et al.S isotopic geo-chemistry,zircon and cassiterite U-Pb geochronology of the Haobugao Sn polymetallic deposit,Southern Great Xing'an Range,NE China[J].Ore Geology Reviews,2018,93:168-180.

[6]

Zhou Q F,Qin K Z,Tang D M,et al.LA-ICP-MS U-Pb zircon,columbite-tantalite and 40Ar-39Ar muscovite age constraints for the rare-element pegmatite dykes in the Altai orogenic belt,NW China[J].Geological Magazine,2018,155(3):707-728.

[7]

曹汇,丛源,李广旭,等.石榴石Lu-Hf、原位独居石U-Pb定年对多期变形的时代制约——以北祁连托勒牧场为例[J].岩石学报,2015,31(12):3755-3768.

Cao H,Cong Y,Li G X,et al.Constrain multistage deformation using garnet Lu-Hf and monazite U-Pb dating:A case study of Tuolemuchang,North Qilian[J].Acta Petrologica Sinica,2015,31(12):3755-3768.

[8]

江思宏,聂凤军,赵省民.铼-锇同位素体系介绍及其在矿床学研究中的应用[J].内蒙古地质,2000(2):47-52. Jiang S H,Nie F J,Zhao X M.An introduction to Re-Os isotopic system and its application to ore study[J].Geology of Inner Mongolia,2000

(2):47-52.

[9]

Selby D,Creaser R A.Macroscale NTIMS and microscale LA-MC-ICP-MS Re-Os isotopic analysis of molybdenite:Testing spatial restrictions for reliable Re-Os age determinations,and implications for the decoupling of Re and Os within molybdenite[J].Geochimica et Cosmochimica Acta,2004,68:3897-3908.

[10]

Pan X F,Hou Z Q,Li Y,et al.Dating the giant Zhuxi W-Cu deposit (Taqian-Fuchun Ore Belt) in South China using molybdenite Re-Os and muscovite Ar-Ar system[J].Ore Geology Reviews,2017,86:719-733.

[11]

Han C M,Xiao W J,Su B X,et al.Geology,Re-Os and U-Pb geochronology and sulfur isotope of the Donggebi porphyry Mo deposit,Xinjiang,NW China,Central Asian Orogenic Belt[J].Journal of Asian Earth Sciences,2018.https://doi.org/10.1016/j.jseaes.2018.05.001.

[12]

Guo W,Zeng Q,Zhang B,et al.Genesis of the Jurassic Dongfengbeishan porphyry Mo deposit in Eastern Yanbian,NE China inferred from molybdenite Re-Os and zircon U-Pb ages,and whole-rock elemental and zircon Hf isotopic compositions[J].Journal of Asian Earth Sciences,2017.https://doi.org/10.1016/j.jseaes.2017.12.035.

[13]

陈衍景,翟明国,蒋少涌.华北大陆边缘造山过程与成矿研究的重要进展和问题[J].岩石学报,2009,25(11):2695-2726.

Chen Y J,Zhai M G,Jiang S Y.Significant achievements and open issues in study of orogenesis and metallogenesis surrounding the North China continent[J].Acta Petrologica Sinica,2009,25(11):2695-2726.

[14]

肖文交,舒良树,高俊,等.中亚造山带大陆动力学过程与成矿作用[J].新疆地质,2008,26(1):4-8.

Xiao W J,Shu L S,Gao J,et al.Continental dynamics of the Central Asian orogenic belt and its metallogeny[J].Xinjiang Geology,2008,26(1):4-8.

[15]

Chen Y J,Pirajno F,Wu G,et al.Epithermal deposits in North Xinjiang,NW China[J].International Journal of Earth Sciences,2012,101(4):889-917.

[16]

Xiao W J,Windley B F,Allen M B,et al.Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage collage[J].Gondwana Research,2013,23(4):1316-1341.

[17]

秦克章,丁奎首,许英霞,等.东天山图拉尔根、白石泉铜镍钴矿床钴、镍赋存状态及原岩含矿性研究[J].矿床地质,2007,26(1):1-14.

Qin K Z,Ding K S,Xu Y X,et al.Ore potential of protoliths and modes of Co-Ni occurrence in Tulargen and Baishiquan Cu-Ni-Co deposits,East Tianshan,Xinjiang[J].Mineral Deposits,2007,26(1):1-14.

[18]

Gao J F,Zhou M F,Qi Liang,et al.Chalcophile elemen-tal compositions and origin of the Tuwu porphyry Cu deposit,NW China[J].Ore Geology Reviews,2015,66:403-421.

[19]

Shen P,Pan H D,Dong L H.Yandong porphyry Cu de-posit,Xinjiang,China-Geology,geochemistry and SIMS U-Pb zircon geochronology of host porphyries and associated alteration and mineralization[J].Journal of Asian Earth Sciences,2014,80:197-217.

[20]

Deng X H,Chen Y J,M Santosh,et al.U-Pb zircon,Re-Os molybdenite geochronology and Rb-Sr geochemistry from the Xiaobaishitou W(-Mo) deposit:Implications for Triassic tectonic setting in Eastern Tianshan,NW China[J].Ore Geology Reviews,2017,80:332-351.

[21]

Chen C,Lü X B,Wu C M,et al.Origin and geodynamic implications of concealed granite in Shadong Tungsten deposit,Xinjiang,China:Zircon U-Pb chronology,geochemistry,and Sr-Nd-Hf isotope constraint[J].Journal of Earth Science,2018,29:114-129.

[22]

Wu Y S,Zhou K F,Li N,et al.Zircon U-Pb dating and Sr-Nd-Pb-Hf isotopes of the ore-associated porphyry at the giant Donggebi Mo deposit,Eastern Tianshan,NW China[J].Ore Geology Reviews,2017,81:794-807.

[23]

Wang Y H,Xu C J,Liu J J,et al.Geological,geoch-ronological,geochemical,and Sr-Nd-O-Hf isotopic constraints on origins of intrusions associated with the Baishan porphyry Mo deposit in eastern Tianshan,NW China[J].Mineralium Deposita,2016,51:953-969.

[24]

陈岳龙,王中刚.新疆东天山花岗岩类的地球化学特征[J].地球化学,1993(3):288-302. Chen Y L,Wang Z G.Geochemical characteristics of east Tianshan granitoid rocks,Xinjiang, China[J].Geochimica,1993

(3):288-302.

[25]

李华芹,陈富文.中国新疆区域成矿作用年代学[M].北京,地质出版社,2004:156-158. Li H Q,Chen F W.Isotopic Geochronology of Regional Mineralization in Xinjiang,NW China[M].Beijing:Geological Publishing House,2004:156

-158.

[26]

李鹏,吕新彪,陈超,等.新疆东天山小白石头黑云母花岗岩年代学、地球化学特征及其地质意义[J].地质与勘探,2011,47(4):543-554.

Li P,Lü X B,Chen C,et al.Geochronology and geochemical characteristics of the biotite-granite in the Xiaobaishitou tungsten deposit,East Tianshan Mountains of Xinjiang and their geological implications[J].Geology and Exploration,2011,47(4):543-554.

[27]

Qin K Z,Su B X,Sakyi P A,et al.SIMS zircon U-Pb geochronology and Sr-Nd isotopes of Ni-Cu bearing mafic-ultramafic intrusions in Eastern Tianshan and Beishan in correlation with flood basalts in Tarim Basin (NW China):Constraints on a ca.280Ma mantle plume[J].American Journal of Science,2011,311(3):237-260.

[28]

Wang Z H,Shu S,Li J,et al.Paleozoic tectonic evolution of the Northern Xinjiang,China:Geochemical and geochronological constrains from the ophiolites[J].Tectonics,2003,22(2):1024.

[29]

王京彬,王玉往,何志军.东天山大地构造演化的成矿示踪[J].中国地质,2006,33(3):461-469.

Wang J B,Wang Y W,He Z J.Ore deposits as a guide to the tectonic evolution in the East Tianshan Mountains,NW China[J].Geology in China,2006,33(3):461-469.

[30]

Tang D M,Qin K Z,Sun H,et al.The role of crustal contamination in the formation of Ni-Cu sulfide deposits in Eastern Tianshan,Xinjiang,Northwest China:Evidence from trace element geochemistry,Re-Os,Sr-Nd,zircon Hf-O,and sulfur isotopes[J].Journal of Asian Earth Sciences,2012,49:145-160.

[31]

李晶,孙亚莉,何克,等.辉钼矿Re-Os同位素定年方法的改进与应用[J].岩石学报,2010,26(2):642-648.

Li J,Sun Y L,He K,et al.The improve molybdebite Re-Os dating method and its application[J].Acta Petrological Sinica,2010,26(2):642-648.

[32]

杜安道,屈文俊,李超,等.铼-锇同位素定年方法及分析测试技术的进展[J].岩矿测试,2009,28(3):288-304.

Du A D,Qu W J,Li C,et al.A review on the development of Re-Os isotopic dating methods and techniques[J].Rock and Mineral Analysis,2009,28(3):288-304.

[33]

黄小文,漆亮,高剑峰,等.关于硫化物Re-Os同位素定年的一些思考[J].矿物岩石地球化学通报,2016,35(3):432-440.

Huang X W,Qi L,Gao J F,et al.Some thoughts on sulfide Re-Os isotope dating[J].Bulletin of Mineralogy,Petrology and Geochemistry,2016,35(3):432-440.

[34]

李杰,张晶,尹露.地质样品的Re-Os同位素分析技术及存在的问题[J].矿物岩石地球化学通报,2018,37(2):242-249.

Li J,Zhang J,Yin L.Advances and problems of Re-Os isotope analysis of geological samples[J].Bulletin of Mineralogy,Petrology and Geochemistry,2018,37(2):242-249.

[35]

Ludwig K R.Squid 1.02:A User's Manual[M].Ber-keley Geochronology Centre,2001:1-219.

[36]

Dong Y P,Zhang G W,Neubauer F,et al.Syn-and post-collisional granitoids in the Central Tianshan orogen:Geochemistry,geochronology and implications for tectonic evolution[J].Gondwana Research,2011,20:568-581.

[37]

Zhang L C,Qin K Z,Xiao W J,et al.Multiple mine-ralization events in the Eastern Tianshan district,NW China:Isotopic geochronology and geological significance[J].Journal of Asian Earth Sciences,2008,32(2-4):236-246.

[38]

李建忠,吴晓智,齐雪峰,等.新疆北部地区上古生界火山岩分布及其构造环境[J].岩石学报,2010,26(1):195-206.

Li J Z,Wu X Z,Qi X F,et al.Distribution and tectonic setting of Upper Paleozoic volcanic rock in the North Xinjiang[J].Acta Petrologica Sinica,2010,26(1):195-206.

[39]

朱江,吕新彪,陈超,等.东天山东段-北山地区三叠纪钼矿床地质特征、时空分布及含矿花岗岩成岩-成矿构造背景[J].新疆地质,2013(1):21-28. Zhu J,Lü

; X B,Chen C,et al.Geological characteristics,spatial and temporal distribution of the Triassic molybdenum deposit in the Eastern Tianshan-Beishan area and the diagenetic-metallogenic tectonic setting of the ore-bearing granite[J].Xinjiang Geology,2013(1):21-28.

[40]

Zhang Z Z,Gu L X,Wu C Z,et al.Zircon SHRIMP dating for the Weiya pluton,Eastern Tianshan:Its geological implications[J].Acta Petrologica Sinica,2005,79:481-490.

[41]

Li H Q,Chen F W,Lu Y F,Yang,et al.New chro-nological evidence for Indosinian diagenetic mineralization in Eastern Xinjiang,NW China[J].Acta Geologica Sinica (English Edition),2005,79(2):264-275.

[42]

吴艳爽,项楠,汤好书,等.东天山东戈壁钼矿床辉钼矿Re-Os年龄及印支期成矿事件[J].岩石学报,2013,29(1):121-130.

Wu Y S,Xiang N,Tang H S,et al.Molybdenite Re-Os isotope age of the Donggebi Mo deposit and the Indosinian metallogenic event in Eastern Tianshan[J].Acta Petrologica Sinica,2013,29(1):121-130.

[43]

Han C M,Xiao W J,Zhao G C,et al.Re-Os Geoch-ronology on molybdenites from the Donggebi Mo deposit in the Eastern Tianshan of the Central Asia orogenic belt and its geological significance[J].Resource Geology,2014,64(2):136-148.

[44]

Sun H S,Li H,Danišík M,et al.U-Pb and Re-Os geochronology and geochemistry of the Donggebi Mo deposit,Eastern Tianshan,NW China:Insights into mineralization and tectonic setting[J].Ore Geology Reviews,2017,86:584-599.

[45]

周涛发,袁峰,张达玉,等.新疆东天山觉罗塔格地区花岗岩类年代学、构造背景及其成矿作用研究[J].岩石学报,2010,26(2):478-502.

Zhou T F,Yuan F,Zhang D Y,et al.Geochronology,tectonic setting and mineralization of granitoids in Jueluotage area,Eastern Tianshan,Xinjiang[J].Acta Petrologica Sinica,2010,26(2):478-502.

[46]

赵宏刚,苏锐,梁积伟,等.中天山东段天湖花岗岩岩石学、地球化学及其成因[J].地质学报,2017,91(6):1208-1226.

Zhao H G,Su R,Liang J W,et al.Petrology,geochemical characteristics and genesis of the Tianhu pluton in the east section of the Middle Tianshan mountains[J].Acta Geologica Sinica,2017,91(6):1208-1226.

[47]

江思宏,聂凤军.甘肃北山红尖兵山钨矿床的40Ar-39Ar同位素年代学研究[J].矿床地质,2006,25(1):89-94.

Jiang S H,Nie F J.40Ar-39Ar geochronology of Hongjianbingshan tungsten deposit in Beishan Mountain,Gansu Province,China[J].Mineral Deposits,2006,25(1):89-94.

[48]

张新虎,苏犁,崔学军,等.甘肃北山造山带玉山钨矿成岩成矿时代及成矿机制[J].科学通报,2008,53(9):1077-1084.

Zhang X H,Su L,Cui X J,et al.Mineralization time and metallogenic mechanism of the Yushan tungsten deposit of the Beishan orogenic belt,Gansu Province[J].Chinese Science Bulletin,2008,53(9):1077-1084.

[49]

张雨莲,许荣科,陕亮,等.内蒙古北山地区小狐狸山钼矿床辉钼矿Re-Os年龄和LA-ICP-MS锆石U-Pb年龄[J].地质通报,2012,31(2-3):469

-475. Zhang Y L,Xu R K,Shan L,et al.Rock-forming and ore-forming ages of the Xiaohulishan molybdenum deposit in Beishan area,Inner Mongolia[J].Geological Bulletin of China,2012,31(2-3):469-475.

[50]

Zhu J,Lü X B,Chen C,et al.U-Pb and Re-Os ages of the Huaheitan Mo deposit in Northwest China[J].Resource Geology,2013,63(3):330-336.

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[9]

罗立强, 马光祖. 辉钼矿中钼,硫,铜,钛,硅等元素的X—射线荧光分析. 岩矿测试, 1989, (2): 95-98.

[10]

杜安道, 屈文俊. 186锇和188锇双同位素稀释法在辉钼矿铼—锇测年中的应用. 岩矿测试, 2000, (4): 241-244.

[11]

杜安道, 屈文俊. 高温密闭溶样电感耦合等离子体质谱准确测定辉钼矿铼-锇地质年龄. 岩矿测试, 2003, (4): 254-257262.

[12]

杜安道, 何红蓼. 铼-锇同位素的等离子体质谱法测定及其在辉钼矿测年中的应用. 岩矿测试, 1993, (3): 161-165.

[13]

赵正, 陈毓川, 陈郑辉, 王登红, 曾载淋, 赵斌, 张家菁. 赣南银坑矿田高山角花岗闪长岩SHRIMP U-Pb定年及其与成矿的关系. 岩矿测试, 2012, 31(3): 536-542.

[14]

黎卫亮, 程秀花, 余娟, 刘欢. 高压密闭酸溶-电感耦合等离子体质谱法测定花岗闪长岩中的微量锆. 岩矿测试, 2016, 35(1): 32-36. doi: 10.15898/j.cnki.11-2131/td.2016.01.006

[15]

应立娟, 林彬, 王立强, 李超, 王阔. 应用电感耦合等离子体质谱法研究西藏甲玛超大型铜多金属矿床辉钼矿稀土元素和微量元素地球化学特征. 岩矿测试, 2015, 34(3): 366-374. doi: 10.15898/j.cnki.11-2131/td.2015.03.018

[16]

夏瑜, 彭光菊, 周卫宁, 张新海, 马荣锴. 江西富家坞矿床铜钼矿石中铼元素的赋存状态及其回收影响因素分析. 岩矿测试, 2017, 36(6): 659-665. doi: 10.15898/j.cnki.11-2131/td.201703270039

[17]

李树昌, 赵建为. 辉钼矿中微量锡的分离与测定. 岩矿测试, 2000, (3): 173-176.

[18]

李玉玲. 辉钼矿单矿物化学全分析. 岩矿测试, 1989, (3): 167-172.

[19]

杜安道, 屈文俊. 中子活化分析在铼—锇法年龄测定中的应用. 岩矿测试, 1997, (4): 289-292.

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Figures And Tables

新疆东天山小白石头钨(钼)矿辉钼矿Re-Os同位素年龄及成矿时代

李宁, 杨富全, 李超, 张志欣, 杨成栋