东昆仑卡而却卡铜钼铁多金属矿床成矿年代学:辉钼矿Re-Os和金云母Ar-Ar同位素定年约束
|
摘要
卡而却卡矿床位于东昆仑祁漫塔格地区,达大型规模,属矽卡岩型矿床,伴有斑岩型和热液型矿化。区内铜钼铁多金属成矿与似斑状二长花岗岩、花岗闪长岩密切相关。B区矽卡岩铜钼矿石由钙铁榴石、符山石、透辉石、方柱石、透闪石、辉钼矿、黄铜矿等组成,辉钼矿Re-Os加权平均年龄为246.1±1.2 Ma(MSWD=0.92),等时线年龄为245.5±1.6 Ma(MSWD=1.2);B区深部矽卡岩型铁矿石中磁铁矿与透闪石、金云母等共生,金云母Ar-Ar坪年龄为233.9±1.4 Ma(MSWD=1.68),反等时线年龄为234.3±1.5 Ma(MSWD=1.58),成矿时代为中-晚三叠世。卡而却卡矿床辉钼矿的Re含量为(1.342±0.014)×10~(-6)~(23.86±0.29)×10~(-6),表明成矿物质为壳幔混合来源。综合区域地质资料,卡而却卡矿床形成于中-晚三叠世碰撞-后碰撞转换阶段,与中-晚三叠世壳幔岩浆混合作用密切相关,壳幔相互作用可能为区域大规模金属成矿提供成矿物质。
The Kaerqueka polymetallic deposit is a large-scale skarn deposit with porphyry and hydrothermal mineralization, which is located at the Qimantage, eastern Kunlun. The copper, molybdenum and iron polymetallic mineralization is closely related with porphyritic monzogranite and granodiorite. The skarn type copper and molybdenum ores are composed of grossular, vesuvianite, diopside, scapolite, tremolite, molybdenite and chalcopyrite. The Re-Os dating of molybdenite yielded a weighted mean age of 246.1±1.2 Ma(MSWD=0.92) and an isochron age of 245.5±1.6 Ma(MSWD=1.2). The phlogopite with paragenesis of magnetite in skran type iron ores yield an Ar-Ar plateau age of 233.9±1.4 Ma(MSWD=1.68) and a diverse isochron age of 234.3±1.5 Ma(MSWD=1.58). The ore forming-age of Kaerqueka deposit was the Middle or Late Triassic era. The Re contents of the molybdenite in the Kaerqueka deposit vary from(1.342±0.014)×10~(-6) to(23.86±0.29)×10~(-6), implying that the ore-forming material was mainly derived from both of crust and mantle. Combing with those available petrogenetic and metallogenic chronological data published recently and regional tectonic research works, it is suggested that the Middle-Late Triassic intrusive rocks in Kaerqueka deposit might be formed by underplating, remelting of ancient crust and magma mixing in the Late Paleozoic to Early Mesozoic collision-post collision stage. The magma mixing at the Middle-Late Triassic era provides a large number of ore-forming materials for large-scale polymetallic mineralization.
The Kaerqueka polymetallic deposit is a large-scale skarn deposit with porphyry and hydrothermal mineralization, which is located at the Qimantage, eastern Kunlun. The copper, molybdenum and iron polymetallic mineralization is closely related with porphyritic monzogranite and granodiorite. The skarn type copper and molybdenum ores are composed of grossular, vesuvianite, diopside, scapolite, tremolite, molybdenite and chalcopyrite. The Re-Os dating of molybdenite yielded a weighted mean age of 246.1±1.2 Ma(MSWD=0.92) and an isochron age of 245.5±1.6 Ma(MSWD=1.2). The phlogopite with paragenesis of magnetite in skran type iron ores yield an Ar-Ar plateau age of 233.9±1.4 Ma(MSWD=1.68) and a diverse isochron age of 234.3±1.5 Ma(MSWD=1.58). The ore forming-age of Kaerqueka deposit was the Middle or Late Triassic era. The Re contents of the molybdenite in the Kaerqueka deposit vary from(1.342±0.014)×10~(-6) to(23.86±0.29)×10~(-6), implying that the ore-forming material was mainly derived from both of crust and mantle. Combing with those available petrogenetic and metallogenic chronological data published recently and regional tectonic research works, it is suggested that the Middle-Late Triassic intrusive rocks in Kaerqueka deposit might be formed by underplating, remelting of ancient crust and magma mixing in the Late Paleozoic to Early Mesozoic collision-post collision stage. The magma mixing at the Middle-Late Triassic era provides a large number of ore-forming materials for large-scale polymetallic mineralization.
引文
谌宏伟,罗照华,莫宣学,刘成东,柯珊.2005.东昆仑造山带三叠纪岩浆混合成因花岗岩的岩浆底侵作用机制.中国地质,32(3):386-395.
杜安道,屈文俊,王登红,李超.2012.铼?锇法及其在矿床学中的应用.北京:地质出版社:1-182.
丰成友,李东生,屈文俊,杜安道,王松,苏生顺,江军.2009.青海祁漫塔格索拉吉尔矽卡岩型铜钼矿床辉钼矿铼?锇同位素定年及其地质意义.岩矿测试,28(3):223-227.
丰成友,李东生,吴正寿,李军红,张占玉,张爱奎,舒晓峰,苏生顺.2010.东昆仑祁漫塔格成矿带矿床类型、时空分布及多金属成矿作用.西北地质,43(4):10-17.
丰成友,王松,李国臣,马圣钞,李东生.2012.青海祁漫塔格中晚三叠世花岗岩:年代学、地球化学及成矿意义.岩石学报,28(2):665-678.
丰成友,王雪萍,舒晓峰,张爱奎,肖晔,刘建楠,马圣钞,李国臣,李大新.2011.青海祁漫塔格虎头崖铅锌多金属矿区年代学研究及地质意义.吉林大学学报(地球科学版),41(6):1806-1817.
高永宝.2013.东昆仑祁漫塔格地区中酸性侵入岩浆活动与成矿作用.西安:长安大学博士学位论文.
高永宝,李侃,钱兵,李文渊,李东生,苏生顺,Chenguang Zhang,张大民,王生明.2015.东昆仑卡而却卡铜矿区花岗闪长岩及其暗色微粒包体成因:锆石U-Pb年龄、岩石化学及Sr-Nd-Hf同位素证据.中国地质,42(3):646-662.
高永宝,李文渊,马晓光,张照伟,汤庆艳.2012.东昆仑尕林格铁矿床成因年代学及Hf同位素制约.兰州大学学报(自然科学版),48(2):36-47.
高永宝,李文渊,钱兵,李侃,李东生,何书跃,张照伟,张江伟.2014a.东昆仑野马泉铁矿相关花岗质岩体年代学、地球化学及Hf同位素特征.岩石学报,30(6):1647-1665.
高永宝,李文渊,钱兵,李侃,张照伟,蒋忠祥,沈灯亮,王志海,叶美芳.2014b.新疆维宝铅锌矿床地质、流体包裹体和同位素地球化学特征.吉林大学学报(地球科学版),44(4):1153-1165.
高永宝,李文渊,谭文娟.2010.祁漫塔格地区成矿地质特征及找矿潜力分析.西北地质,43(4):35-43.
郭正府,邓晋福,许志琴,莫宣学,罗照华.1998.青藏东昆仑晚古生代末?中生代中酸性火成岩与陆内造山过程.现代地质,12(3):344-352.
侯增谦,曲晓明,王淑贤,高永丰,杜安道,黄卫.2003.西藏高原冈底斯斑岩铜矿带辉钼矿Re-Os年龄:成矿作用时限与动力学背景应用.中国科学(D辑),33(7):609-618.
黄典豪,杜安道,吴澄宇,刘兰笙,孙亚莉,邹晓秋.1996.华北地台钼(铜)矿床成矿学研究:辉钼矿的铼?锇年龄及其地质意义.矿床地质,15(4):289-297.
黄典豪,吴澄宇,杜安道,何红蓼.1994.东秦岭地区钼矿床的铼?锇同位素年龄及其意义.矿床地质,13(3):221-230.
李大新,丰成友,赵一鸣,李泽峰,刘建楠,肖晔.2011.青海卡而却卡铜多金属矿床蚀变矿化类型及矽卡岩矿物学特征.吉林大学学报(地球科学版),41(6):1818-1830.
李东生.2012.青海省东昆仑成矿带斑岩型矿床成矿规律及找矿前景.北京:中国地质大学(北京)博士学位论文.
李红艳,毛景文,孙亚莉,邹晓秋,何红蓼,杜安道.1996.柿竹园钨多金属矿床的Re-Os同位素等时线年龄研究.地质论评,42(3):261-267.
李侃,高永宝,钱兵,何书跃,刘永乐,张照伟,张江伟,王亚磊.2015.东昆仑祁漫塔格虎头崖铅锌多金属矿区花岗岩年代学、地球化学及Hf同位素特征.中国地质,42(3):630-643.
李荣社,计文化,杨永成.2008.昆仑山及邻区地质.北京:地质出版社:1-400.
李世金,孙丰月,王力,李玉春,刘振宏,苏生顺,王松.2008.青海东昆仑卡尔却卡多金属矿区斑岩型铜矿的流体包裹体研究.矿床地质,27(3):399-406.
刘成东,莫宣学,罗照华,喻学惠,谌宏伟,李述为,赵欣.2003.东昆仑造山带花岗岩Pb-Sr-Nd-O同位素特征.地球学报,24(6):584-588.
刘成东,张文秦,莫宣学,罗照华,喻学惠,李述为,赵欣.2002.东昆仑约格鲁岩体暗色微粒包体特征与成因.地质通报,21(11):739-744.
刘红涛.2001.祁漫塔格陆相火山岩:塔里木陆块南缘印支期活动大陆边缘的岩石学证据.岩石学报,17(3):337-351.
罗照华,柯珊,曹永清,邓晋福,柯珊,谌宏伟.2002.东昆仑印支晚期幔源岩浆活动.地质通报,21(6):292-297.
莫宣学,罗照华,邓晋福,喻学惠,刘成东,谌宏伟,袁万明,刘云华.2007.东昆仑造山带花岗岩及地壳生长.高校地质学报,13(3):403-414.
孟祥金,侯增谦,高永丰,黄卫,曲晓明,屈文俊.2003.西藏冈底斯成矿带驱龙铜矿Re-Os年龄及成矿学意义.地质论评,49(6):660-666.
南卡俄吾,贾群子,李文渊,郭周平,李金超,孔会磊,栗亚芝,代岩.2014.青海东昆仑哈西亚图铁多金属矿区石英闪长岩LA-ICP-MS锆石U-Pb年龄和岩石地球化学特征.西北地质,33(6):841-849.
钱兵,高永宝,李侃,张照伟,周安顺,吴玉诗.2015.新疆东昆仑于沟子地区与铁?稀有多金属成矿有关的碱性花岗岩地球化学、年代学及Hf同位素研究.岩石学报,31(9):2508-2520.
青海省地质调查研究院.2004.1∶5万水泥厂幅、忠阳山幅、黑刺沟幅区域地质调查报告.
青海省第三地质矿产勘查院.2013.青海省格尔木市卡而却卡地区铜多金属矿整装勘查成果报告.
任继舜,姜春发,张正坤,秦德余.1980.中国大地构造及其演化.北京:科学出版社:1-124.
佘宏全,张德全,景向阳,关军,朱华平,丰成友,李大新.2007.青海省乌兰乌珠尔斑岩铜矿床地质特征与成因.中国地质,34(2):306-314.
宋文彬,赖健清,黄敏,杨自安,张普斌,欧阳华平.2012.青海省卡尔却卡铜多金属矿床流体包裹体特征及成矿流体.中国有色金属学报,22(3):733-742.
田承盛,丰成友,李军红,曹德智.2013.青海它温查汉铁多金属矿床40Ar-39Ar年代学研究及意义.矿床地质,32(1):169-176.
王富春,陈静,谢志勇,李善平,谈生祥,张玉宝,王涛.2013.东昆仑拉陵灶火钼多金属矿床地质特征及辉钼矿Re-Os同位素定年.中国地质,40(4):1209-1217.
王松,丰成友,李世金,江军华,李东生,苏生顺.2009.青海祁漫塔格卡尔却卡铜多金属矿区花岗闪长岩锆石SHRIMP U-Pb测年及其地质意义.中国地质,36(1):74-84.
吴祥珂,孟繁聪,许虹,崔美慧.2011.青海祁漫塔格玛兴大坂晚三叠世花岗岩年代学、地球化学及Nd-Hf同位素组成.岩石学报,27(11):3380-3394.
肖晔,丰成友,刘建楠,于淼,周建厚,李大新,赵一鸣.2013.青海肯德可克铁多金属矿区年代学及硫同位素特征.矿床地质,32(1):177-186.
殷鸿福,张克信.1998.中央造山带的演化及其特点.地球科学,23(5):437-442.
于淼,丰成友,刘洪川,李定武,赵一鸣,李大新,刘建楠,王辉,张明辉.2015.青海尕林格矽卡岩型铁矿金云母40Ar/39Ar年代学及成矿地质意义.地质学报,89(3):510-521.
袁万明,莫宣学,喻学惠,罗照华.2000.东昆仑印支期区域构造背景的花岗岩记录.地质论评,46(2):203-211.
张爱奎,莫宣学,李云平,吕军,曹永亮,舒晓峰,李华.2010.青海西部祁漫塔格成矿带找矿新进展及其意义.地质通报,29(7):1062-1074.
周建厚,丰成友,王辉,周安顺.2014.新疆祁漫塔格于沟子铁多金属矿辉钼矿Re-Os年龄及其地质意义.地质与勘探,50(1):1-7.
Koppers A A P.2002.Ar Ar CALC-Software for 40Ar/39Ar age calculations.Computers and Geosciences,28:605-619.
Ludwig K R.2003.User’s manual for isotoplot 3.1,Ageochronological toolkit for Microsoft Excle.Berkeley Geochronology Center Special Publication,4:25-32.
Mao J W,Zhang Z C and Zhang Z H.1999.Re-Os isotopic dating of molybdenites in the Xiaoliugou W(Mo)deposit in the northern Qilian Mountains and its geological significance.Geochimica et Cosmochimica Acta,63(11?12):1815-1818.
Smoliar M I,Walker R J and Morgan J W.1996.Re-Os ages of group IIA,IIIA,IVA and VIB iron meteorites.Science,271:1099-1102.
Steiger R H and J?ger E.1977.Subcommission on geochronology:Convention on the use of decay constants in geo-and cosmochronology.Earth and Planetary Science Letters,36:359-362.
Stein H J,Markey R J,Morgan J W and Scherstén A.2001.The remarkable Re-Os chronometer inmolybdenite:How and why it works.Terra Nova,13(6):479-486.
Wang F,Jourdan F,Lo C H,Nomade S,Guillou H,Zhu R X,Yang L,Shi W,Feng H,Wu L and Sang H.2014.YBCs:A new standard for 40Ar/39Ar dating.Chemical Geology,388:87-98.
Yang L K,Wang F,Shen J L,Chen R and Xing G F.2008.Lasing on pyroclastic rocks:A case study of 40Ar/39Ar dating on Moshishan Group,eastern Zhejiang Province.Chinese Science Bulletin,53(24):3876-3882.
杜安道,屈文俊,王登红,李超.2012.铼?锇法及其在矿床学中的应用.北京:地质出版社:1-182.
丰成友,李东生,屈文俊,杜安道,王松,苏生顺,江军.2009.青海祁漫塔格索拉吉尔矽卡岩型铜钼矿床辉钼矿铼?锇同位素定年及其地质意义.岩矿测试,28(3):223-227.
丰成友,李东生,吴正寿,李军红,张占玉,张爱奎,舒晓峰,苏生顺.2010.东昆仑祁漫塔格成矿带矿床类型、时空分布及多金属成矿作用.西北地质,43(4):10-17.
丰成友,王松,李国臣,马圣钞,李东生.2012.青海祁漫塔格中晚三叠世花岗岩:年代学、地球化学及成矿意义.岩石学报,28(2):665-678.
丰成友,王雪萍,舒晓峰,张爱奎,肖晔,刘建楠,马圣钞,李国臣,李大新.2011.青海祁漫塔格虎头崖铅锌多金属矿区年代学研究及地质意义.吉林大学学报(地球科学版),41(6):1806-1817.
高永宝.2013.东昆仑祁漫塔格地区中酸性侵入岩浆活动与成矿作用.西安:长安大学博士学位论文.
高永宝,李侃,钱兵,李文渊,李东生,苏生顺,Chenguang Zhang,张大民,王生明.2015.东昆仑卡而却卡铜矿区花岗闪长岩及其暗色微粒包体成因:锆石U-Pb年龄、岩石化学及Sr-Nd-Hf同位素证据.中国地质,42(3):646-662.
高永宝,李文渊,马晓光,张照伟,汤庆艳.2012.东昆仑尕林格铁矿床成因年代学及Hf同位素制约.兰州大学学报(自然科学版),48(2):36-47.
高永宝,李文渊,钱兵,李侃,李东生,何书跃,张照伟,张江伟.2014a.东昆仑野马泉铁矿相关花岗质岩体年代学、地球化学及Hf同位素特征.岩石学报,30(6):1647-1665.
高永宝,李文渊,钱兵,李侃,张照伟,蒋忠祥,沈灯亮,王志海,叶美芳.2014b.新疆维宝铅锌矿床地质、流体包裹体和同位素地球化学特征.吉林大学学报(地球科学版),44(4):1153-1165.
高永宝,李文渊,谭文娟.2010.祁漫塔格地区成矿地质特征及找矿潜力分析.西北地质,43(4):35-43.
郭正府,邓晋福,许志琴,莫宣学,罗照华.1998.青藏东昆仑晚古生代末?中生代中酸性火成岩与陆内造山过程.现代地质,12(3):344-352.
侯增谦,曲晓明,王淑贤,高永丰,杜安道,黄卫.2003.西藏高原冈底斯斑岩铜矿带辉钼矿Re-Os年龄:成矿作用时限与动力学背景应用.中国科学(D辑),33(7):609-618.
黄典豪,杜安道,吴澄宇,刘兰笙,孙亚莉,邹晓秋.1996.华北地台钼(铜)矿床成矿学研究:辉钼矿的铼?锇年龄及其地质意义.矿床地质,15(4):289-297.
黄典豪,吴澄宇,杜安道,何红蓼.1994.东秦岭地区钼矿床的铼?锇同位素年龄及其意义.矿床地质,13(3):221-230.
李大新,丰成友,赵一鸣,李泽峰,刘建楠,肖晔.2011.青海卡而却卡铜多金属矿床蚀变矿化类型及矽卡岩矿物学特征.吉林大学学报(地球科学版),41(6):1818-1830.
李东生.2012.青海省东昆仑成矿带斑岩型矿床成矿规律及找矿前景.北京:中国地质大学(北京)博士学位论文.
李红艳,毛景文,孙亚莉,邹晓秋,何红蓼,杜安道.1996.柿竹园钨多金属矿床的Re-Os同位素等时线年龄研究.地质论评,42(3):261-267.
李侃,高永宝,钱兵,何书跃,刘永乐,张照伟,张江伟,王亚磊.2015.东昆仑祁漫塔格虎头崖铅锌多金属矿区花岗岩年代学、地球化学及Hf同位素特征.中国地质,42(3):630-643.
李荣社,计文化,杨永成.2008.昆仑山及邻区地质.北京:地质出版社:1-400.
李世金,孙丰月,王力,李玉春,刘振宏,苏生顺,王松.2008.青海东昆仑卡尔却卡多金属矿区斑岩型铜矿的流体包裹体研究.矿床地质,27(3):399-406.
刘成东,莫宣学,罗照华,喻学惠,谌宏伟,李述为,赵欣.2003.东昆仑造山带花岗岩Pb-Sr-Nd-O同位素特征.地球学报,24(6):584-588.
刘成东,张文秦,莫宣学,罗照华,喻学惠,李述为,赵欣.2002.东昆仑约格鲁岩体暗色微粒包体特征与成因.地质通报,21(11):739-744.
刘红涛.2001.祁漫塔格陆相火山岩:塔里木陆块南缘印支期活动大陆边缘的岩石学证据.岩石学报,17(3):337-351.
罗照华,柯珊,曹永清,邓晋福,柯珊,谌宏伟.2002.东昆仑印支晚期幔源岩浆活动.地质通报,21(6):292-297.
莫宣学,罗照华,邓晋福,喻学惠,刘成东,谌宏伟,袁万明,刘云华.2007.东昆仑造山带花岗岩及地壳生长.高校地质学报,13(3):403-414.
孟祥金,侯增谦,高永丰,黄卫,曲晓明,屈文俊.2003.西藏冈底斯成矿带驱龙铜矿Re-Os年龄及成矿学意义.地质论评,49(6):660-666.
南卡俄吾,贾群子,李文渊,郭周平,李金超,孔会磊,栗亚芝,代岩.2014.青海东昆仑哈西亚图铁多金属矿区石英闪长岩LA-ICP-MS锆石U-Pb年龄和岩石地球化学特征.西北地质,33(6):841-849.
钱兵,高永宝,李侃,张照伟,周安顺,吴玉诗.2015.新疆东昆仑于沟子地区与铁?稀有多金属成矿有关的碱性花岗岩地球化学、年代学及Hf同位素研究.岩石学报,31(9):2508-2520.
青海省地质调查研究院.2004.1∶5万水泥厂幅、忠阳山幅、黑刺沟幅区域地质调查报告.
青海省第三地质矿产勘查院.2013.青海省格尔木市卡而却卡地区铜多金属矿整装勘查成果报告.
任继舜,姜春发,张正坤,秦德余.1980.中国大地构造及其演化.北京:科学出版社:1-124.
佘宏全,张德全,景向阳,关军,朱华平,丰成友,李大新.2007.青海省乌兰乌珠尔斑岩铜矿床地质特征与成因.中国地质,34(2):306-314.
宋文彬,赖健清,黄敏,杨自安,张普斌,欧阳华平.2012.青海省卡尔却卡铜多金属矿床流体包裹体特征及成矿流体.中国有色金属学报,22(3):733-742.
田承盛,丰成友,李军红,曹德智.2013.青海它温查汉铁多金属矿床40Ar-39Ar年代学研究及意义.矿床地质,32(1):169-176.
王富春,陈静,谢志勇,李善平,谈生祥,张玉宝,王涛.2013.东昆仑拉陵灶火钼多金属矿床地质特征及辉钼矿Re-Os同位素定年.中国地质,40(4):1209-1217.
王松,丰成友,李世金,江军华,李东生,苏生顺.2009.青海祁漫塔格卡尔却卡铜多金属矿区花岗闪长岩锆石SHRIMP U-Pb测年及其地质意义.中国地质,36(1):74-84.
吴祥珂,孟繁聪,许虹,崔美慧.2011.青海祁漫塔格玛兴大坂晚三叠世花岗岩年代学、地球化学及Nd-Hf同位素组成.岩石学报,27(11):3380-3394.
肖晔,丰成友,刘建楠,于淼,周建厚,李大新,赵一鸣.2013.青海肯德可克铁多金属矿区年代学及硫同位素特征.矿床地质,32(1):177-186.
殷鸿福,张克信.1998.中央造山带的演化及其特点.地球科学,23(5):437-442.
于淼,丰成友,刘洪川,李定武,赵一鸣,李大新,刘建楠,王辉,张明辉.2015.青海尕林格矽卡岩型铁矿金云母40Ar/39Ar年代学及成矿地质意义.地质学报,89(3):510-521.
袁万明,莫宣学,喻学惠,罗照华.2000.东昆仑印支期区域构造背景的花岗岩记录.地质论评,46(2):203-211.
张爱奎,莫宣学,李云平,吕军,曹永亮,舒晓峰,李华.2010.青海西部祁漫塔格成矿带找矿新进展及其意义.地质通报,29(7):1062-1074.
周建厚,丰成友,王辉,周安顺.2014.新疆祁漫塔格于沟子铁多金属矿辉钼矿Re-Os年龄及其地质意义.地质与勘探,50(1):1-7.
Koppers A A P.2002.Ar Ar CALC-Software for 40Ar/39Ar age calculations.Computers and Geosciences,28:605-619.
Ludwig K R.2003.User’s manual for isotoplot 3.1,Ageochronological toolkit for Microsoft Excle.Berkeley Geochronology Center Special Publication,4:25-32.
Mao J W,Zhang Z C and Zhang Z H.1999.Re-Os isotopic dating of molybdenites in the Xiaoliugou W(Mo)deposit in the northern Qilian Mountains and its geological significance.Geochimica et Cosmochimica Acta,63(11?12):1815-1818.
Smoliar M I,Walker R J and Morgan J W.1996.Re-Os ages of group IIA,IIIA,IVA and VIB iron meteorites.Science,271:1099-1102.
Steiger R H and J?ger E.1977.Subcommission on geochronology:Convention on the use of decay constants in geo-and cosmochronology.Earth and Planetary Science Letters,36:359-362.
Stein H J,Markey R J,Morgan J W and Scherstén A.2001.The remarkable Re-Os chronometer inmolybdenite:How and why it works.Terra Nova,13(6):479-486.
Wang F,Jourdan F,Lo C H,Nomade S,Guillou H,Zhu R X,Yang L,Shi W,Feng H,Wu L and Sang H.2014.YBCs:A new standard for 40Ar/39Ar dating.Chemical Geology,388:87-98.
Yang L K,Wang F,Shen J L,Chen R and Xing G F.2008.Lasing on pyroclastic rocks:A case study of 40Ar/39Ar dating on Moshishan Group,eastern Zhejiang Province.Chinese Science Bulletin,53(24):3876-3882.