粤东塌山斑岩型锡多金属矿床锆石及锡石U-Pb年代学、Hf同位素组成及其地质意义
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摘要
陆河县塌山斑岩型锡多金属矿床位于粤东地区莲花山断裂带南西段,是粤东锡多金属成矿带内与花岗斑岩和石英斑岩密切相关的锡矿床,同时也是全国三个典型斑岩型锡矿之一。本文对与矿化有关的花岗斑岩进行了锆石U-Pb年代学和Hf同位素综合研究。LA-ICP-MS锆石U-Pb定年显示,花岗斑岩侵位年龄为136.8±1.1 Ma,是早白垩世岩浆作用产物。同时本文对锡石进行了U-Pb定年研究,27个数据在~(206)Pb/~(238)U-~(207)Pb/~(238)U谐和年龄图上获得了133.6±8.6 Ma的下交点年龄,在Tera-Wasserburg年龄图解上获得了136.5±8.1 Ma的下交点年龄,两年龄在误差范围内一致,且与花岗斑岩年龄一致,很好的限定了塌山矿区成矿时代。花岗斑岩锆石εHf(t)从-4.87变化到-2.07,二阶段模式年龄(t_(DM2))为1322～1507 Ma,表明其成岩物质主要来自中元古代地壳岩石,可能有少量地幔物质加入。
The Tashan porphyry tin polymetallic deposit is located at the southwest part of the Lianhuashan Fault in the eastern Guangdong province. It is one of the three typical porphyry tin deposits in China. In this paper, we reported cassiterite and zircon U-Pb ages, geochemistry and Lu-Hf isotopes of the ore-bearing granite porphyry in the orefield. Zircon LA-ICP-MS U-Pb dating yielded a concordant ages of 136.8±1.1 Ma, whereas analyses of cassiterite yielded a ~(206)Pb/~(238) U-~(207) Pb/~(238) U concordia lower intercept age of 133.6±8.6 Ma and a Tera-Wasserburg lower intercept age of 136.5±8.1 Ma, which suggest a genetic link between the granite porphyry and the ore mineralization. The ε_(Hf)(t) values of-4.87 to-2.07 and t_(DM)2 ages 1322 Ma to 1507 Ma for zircon from the granite porphyry show that the Tashan granite porphyry was likely derived from partial melting of the Mesoproterozoic crustal rocks with minor input of mantle material.
The Tashan porphyry tin polymetallic deposit is located at the southwest part of the Lianhuashan Fault in the eastern Guangdong province. It is one of the three typical porphyry tin deposits in China. In this paper, we reported cassiterite and zircon U-Pb ages, geochemistry and Lu-Hf isotopes of the ore-bearing granite porphyry in the orefield. Zircon LA-ICP-MS U-Pb dating yielded a concordant ages of 136.8±1.1 Ma, whereas analyses of cassiterite yielded a ~(206)Pb/~(238) U-~(207) Pb/~(238) U concordia lower intercept age of 133.6±8.6 Ma and a Tera-Wasserburg lower intercept age of 136.5±8.1 Ma, which suggest a genetic link between the granite porphyry and the ore mineralization. The ε_(Hf)(t) values of-4.87 to-2.07 and t_(DM)2 ages 1322 Ma to 1507 Ma for zircon from the granite porphyry show that the Tashan granite porphyry was likely derived from partial melting of the Mesoproterozoic crustal rocks with minor input of mantle material.
引文
白玉珍,满发胜,倪守斌,黎彤.1983.莲花山钨矿区K-Ar同位素地质年龄.地球化学,(2):133-139.
陈毓川,王登红,徐志刚,黄凡.2014.华南区域成矿和中生代岩浆成矿规律概要.大地构造与成矿学,38(2):219-229.
广东省地质局756大队.1985.广东省陆丰县塌山锡矿床详查报告.
华仁民,陈培荣,张文兰,陆建军.2005.论华南地区中生代3次大规模成矿作用.矿床地质,24(2):99-107.
华仁民,李光来,张文兰,胡东泉,陈培荣,陈卫锋,王旭东.2010.华南钨和锡大规模成矿作用的差异及其原因初探.矿床地质,29(1):9-23.
李海立,肖惠良,范飞鹏,陈乐柱,刘建雄,陈叙涛通.2016.广东潮安飞鹅山钨钼多金属矿床辉钼矿Re-Os同位素定年.地质学报,90(2):231-239
李建超,丘元禧.1990.广东莲花山燕山早期断裂动热变质带的基本特征及形成机制的探讨.长春地质学院学报,20(1):93-106.
刘鹏,程彦博,毛景文,王小雨,姚薇,陈叙涛,曾晓剑.2015.粤东田东钨锡多金属矿床花岗岩锆石U-Pb年龄、Hf同位素特征及其意义.地质学报,89(7):1244-1257.
刘师先.1992.塌山斑岩锡矿床地质特征及成矿机理.地球化学,(2):149-157.
路远发.1997.广东钟丘洋次火山岩型铜矿床蚀变围岩的岩石化学特征.华南地质与矿产,(3):1-6.
满发胜,白玉珍,倪守斌,黎彤.1983.莲花山钨矿床同位素地质学初步研究.矿床地质,4(1):35-42.
毛景文,谢桂青,郭春丽,袁顺达,程彦博,陈毓川.2008.华南地区中生代主要金属矿床时空分布规律和成矿环境.高校地质学报,14(4):510-526.
戚建中,黄宾.1988.粤东长埔一西岭地区锡矿断裂岩浆控制因素及成矿模式.中国地质科学院南京矿产地质研究所所刊,9(4):76-94.
丘元禧,丘津松,李建超,钟宏平.1991.广东莲花山断裂带中、新生代多期复合变形变质带的基本特征及其形成机制的探讨.中国地质科学院地质力学研究所所刊,14:93-106
丘增旺,王核,汪礼明,卜安,李莎莎,闫庆贺,暮生禄,李沛,魏小鹏.2016.广东长埔锡多金属矿床石英斑岩锆石U-Pb年代学、Hf同位素组成及其地质意义.地球化学,45(4):374-386.
沈渭洲,凌洪飞.1994.岩背和塌山含锡花岗斑岩的同位素地球化学特征和物质来源.地球学报(1-2):117-123.
涂湘林,张红,邓文峰,凌明星,梁华英,刘颖,孙卫东.2011.RESOlution激光剥蚀系统在微量元素原位微区分析中的应用.地球化学,40(1):83-98.
王德滋,陈绍海,刘昌实,沈渭洲,楚雪君.1995.粤东塌山含锡花岗斑岩原生铝质矿物特征和成因.矿物学报,15(3):249-253.
王小雨.粤东新寮岽铜多金属矿床地质特征及成因初步研究.2015.北京:中国地质大学(北京)硕士学位论文:1-88.
王志强,陈斌,马星华.2014.南岭芙蓉锡矿田锡石原位LA-ICP-MS U-Pb年代学及地球化学研究:对成矿流体来源和演化的意义.科学通报,59(25):2505-2519.
吴福元,李献华,郑永飞,高山.2007.Lu-Hf同位素体系及其岩石学应用.岩石学报,23(2):185-220.
吴淦国,张达,彭润民,吴建设,高天钧,陈柏林等.2004.东南沿海成矿带矿床形成的时间演化规律研究.地学前缘,11(1):237-247.
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589-1604.
徐晓春,岳书仓.1994a.粤东地区中生代火山岩与侵入岩的成因关系及成因类型.合肥工业大学学报(自然科学版),17(4):184-192.
徐晓春,岳书仓.1994b.粤东地区锡多金属矿床的成矿年龄和矿床成因//中国矿物岩石地球化学研究新进展.兰州:兰州大学出版社:347-348.
徐晓春,岳书仓.1996.粤东地区中生代岩浆作用的大地构造背景及构造-岩浆演化.合肥工业大学学报(自然科学版),19(1):127-134.
徐晓春,岳书仓.1999a.粤东锡(钨、铜)多金属矿床的成矿物质来源和成矿作用.地质科学,34(1):81-92.
徐晓春,岳书仓.1999b.粤东中生代花岗质火山-侵入杂岩成因的Nd同位素制约.合肥工业大学学报(自然科学版),22(3):3-6.
徐晓春,岳书仓.1999c.粤东中生代火山-侵入杂岩的地壳深熔成因--Pb-Nd-Sr多元同位素体系制约.地质论评,45(S1):829-835.
岳书仓,雷新勇,龚昌瑞,徐晓春.1989.粤东花岗岩及锡、钨矿床的地球化学研究.中国地质科学院南京地质矿产研究所所刊,10(1):27-41.
邹和平,王建华,丘元禧.2000.广东南澳和莲花山韧性剪切带40Ar/39Ar年龄及其地质意义.地球学报,21(4):356-364.
Amelin Y,Lee D C,Halliday A N,Pidgeon R T.1999.Nature of the Earth’s earliest crust from hafnium isotopes in single detrital zircons.Nature,399(6733):252-255.
Belousova E A,Griffin W L,Suzanne Y,O’Reilly and Fisher N I.2002.Igneous zircon:Trace element composition as an indicator of source rock type.Contributions to Mineralogy and Petrology,143(5):602-622.
Black L P,Kamo S L,Allen C M,Aleinikoff J N,Davis D W,Korsch R J and Foudoulis C.2003.TEMORA 1:A new zircon standard for Phanerozoic U-Pb geochronology.Chemical Geology,200(1):155-170.
Blichert-Toft J and Albarede F.1997.The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle crust system.Earth and Planetary Science Letters,148(1-2):243-258.
Chen X C,Hu R Z,Bi X W,Li H M,Lan J B,Zhao C H and Zhu J J.2014.Cassiterite LA-(MC)ICP-MS U/Pb and muscovite 40Ar/39Ar dating of tin deposits in the Tengchong-Lianghe tin district,NW Yunnan,China.Mineralium Deposita,49(7):843-860.
Chu N C,Taylor R N,Chavagnac V,Nesbitt R W,Boella RM,Milton J A,German C,Bayon G and Burton K.2002.Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry:An evaluation of isobaric interference corrections.Journal of Analytical Atomic Spectrometry,17(12):1567-1574.
Griffin W L,Wang X,Jackson S E,Pearson N J and O’Reilly S Y.2002.Zircon geochemistry and magma mixing,SE China:In-situ analysis of Hf isotopes,Tonglu and Pingtan igneous complexes.Lithos,61(3-4):237-269.
Gulson B L and Jones M T.1992.Cassiterite-potential for direct dating of mineral-deposits and a precise age for the Bushveld complex granites.Geology,20(4):355-358.
Guo F,Fan W M,Li C W,Zhao L,Li H X and Yang J H.2012.Multi-stage crust-mantle interaction in SE China:Temporal,thermal and compositional constraints from the Mesozoic felsic volcanic rocks in eastern GuangdongFujian provinces.Lithos,150:62-84.
Hu R Z and Zhou M F.2012.Multiple Mesozoic mineralization events in South China-an introduction to the thematic issue.Mineralium Deposita,47(6):579-588.
Jiang S Y,Yu J M and Lu J J.2004.Trace and rare-earth element geochemistry in tourmaline and cassiterite from the Yunlong tin deposit,Yunan,China:Implication for migmatitic-hydrothermal fluid evolution and ore genesis.Chemical Geology,209:193-213
Li C Y,Zhang R Q,Ding X,Ling M X,Fan W M and Sun WD.2015.Dating cassiterite using laser ablation ICP-MS.Ore Geology Reviews,72:313-322.
Li X,Long W,Li Q,Liu Y,Zheng Y,Yang Y,Chamberlain KR,Wan D,Guo C and Wang X.2010.Penglai zircon megacrysts:A potential new working reference material for microbeam determination of Hf-O isotopes and U-Pb age.Geostandards and Geoanalytical Research,34(2):117-134.
Liu Y P,Li Z X,Li H M,Guo L G,Xu W,Ye L,Li C Y and Pi D H.2007.U-Pb geochronology of cassiterite and zircon from the Dulong Sn-Zn deposit:Evidence for Cretaceous large-scale granitic magmatism and mineralization events in southeastern Yunnan province,China.Acta Petrological Sinaca,23(5):967-976.
Liu Y S,Hu Z C,Gao S,Günther D,Xu J,Gao C G and Chen H H.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43.
Ludwig,K.R.,2003.User’s Manual for Isoplot 3.00:AGeochronological Toolkit for Microsoft Excel.Berkeley:Berkeley Geochronology Center:1-70.
Ma N,Deng J,Wang Q F,Wang C M,Zhang J and Li GJ.2013.Geochronology of the Dasongpo tin deposit,Yunnan Province:Evidence from zircon LA-ICP-MSU-Pb ages and cassiterite LA-MC-ICP-MS U-Pb age.Acta Petrological Sinaca,29(4),1223-1235.
Mao J W,Cheng Y B,Chen M H and Pirajno F.2013.Major types and time-space distribution of Mesozoic ore deposits in South China and their geodynamic settings.Mineralium Deposita,48(3):267-294.
Mao J W,Pirajno F and Cook N.2011.Mesozoic metallogeny in East China and corresponding geodynamic settingsAn introduction to the special issue.Ore Geology Reviews,43(1):1-7.
Plimer I R,Lu J and Kleeman J D.1991.Trace and rare earth elements in cassiterite-sources of components for the tin deposits of the Mole Granite,Australia.Mineralium Deposita,26:267-274.
Qiu Z W,Li S S,Yan Q H,Wang H,Wei X P,Li P and Bu A.2017a.Late Jurassic Sn metallogeny in eastern Guangdong,SE China coast:Evidence from geochronology,geochemistry and Sr-Nd-Hf-S isotopes of the Dadaoshan Sn deposit.Ore Geology Reviews,83:63-83.
Qiu Z W,Yan Q H,Li S S,Wang H,Tong L X,Zhang R Q,Wei X P,Li P,Wang L M,Bu A and Yan L M.2017b.Highly fractionated Early Cretaceous I-type granites and related Sn polymetallic mineralization in the Jinkeng deposit,eastern Guangdong,SE China:Constraints from geochronology,geochemistry,and Hf isotopes.Ore Geology Reviews,88:718-738.
Rubatto D and Gebauer D.2000.Use of cathodoluminescence for U-Pb zircon dating by ion microprobe:Some examples from the Western Alps//Pagel M,Barbin V,Blanc P and Ohnenstetter D.Cathodoluminescence in Geosciences.Springer Berlin Heidelberg:373-400.
Scherer E,Munker C and Mezger K.2001.Calibration of the lutetium-hafnium clock.Science,293:683-687.
Wang X J,Liu Y P,Miao Y L,Bao T,Ye L and Zhang Q.2014.In-situ LA-MC-ICP-MS cassiterite U-Pb dating of Dulong Sn-Zn polymetallic deposit and its signifycance.Acta Petrologica Sinica,30(3):867-876.
Wu F Y,Yang Y H,Xie L W,Yang J H and Xu P.2006.Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology.Chemical Geology,234(1-2):105-126.
Xie L W,Yin Q Z,Yang J H,Wu F Y and Yang Y H.2013.A tin-mineralized topaz rhyolite dike with coeval topaz granite enclaves at Qiguling in the Qitianling tin district,southern China.Lithos,170:252-268.
Yan Q H,Li S S,Qiu,Z W,Wang H,Wei X P,Dong R and Zhang X Y.2017.Geochronology,geochemistry and Sr-Nd-Hf-S-Pb isotopes of the early cretaceous Taoxihu Sn deposit and related granitoids,SE China.Ore Geology Reviews,89:350-368.
Yan Q H,Qi Z W,Wang H,Wang M,Wei X P,Li P,Zhang RQ,Li C Y and Liu J P.2016.Age of the Dahongliutan rare metal pegmatite deposit,West Kunlun,Xinjiang(NWChina):Constraints from LA-ICP-MS U-Pb dating of columbite-(Fe)and cassiterite.Ore Geology Reviews,http://dx.doi.org/10.1016/j.oregeorev.2016.11.010
Yan Q H,Wang H,Qiu Z W,Wei X P,Li P,Dong R and Zhou K L.2018.Origin of Early Cretaceous A-type granite and related Sn mineralization in the Sanjiaowo deposit,eastern Guangdong,SE China and its tectonic implication.Ore Geology Reviews,93:60-80.
Yuan S D,Peng J T,Hu R Z,Li H M,Shen N P and Zhang DL.2008.A precise U-Pb age on cassiterite from the Xianghualing tin-polymetallic deposit,Hunan,South China.Mineralium Deposita,43:375-382.
Yuan S D,Peng J T,Hu R Z,Li H M,Shen N P and Zhang DL.2011.In situ LA-MC-ICP-MS and ID-TIMS U-Pb geochronology of cassiterite in the giant Furong tin deposit,Hunanb Province,South China:New constraints on the timing of tin-polymetallic mineralization.Ore Geology Reviews,43(1):235-242.
Zhang D L,Peng J T,Coulson I M,Hou L H and Li S J.2014.Cassiterite U-Pb and muscovite 40Ar-39Ar age constraints on the timing of mineralization in the Xuebaoding Sn-W-Be deposit,western China.Ore Geology Reviews,62:315-322.
Zhang R Q,Lu J J,Wang R C,Lu X C,Guo J C,Li F C,Lehmann B,Yao Y and Guo W M.2013.Contrasting Wand Sn mineralization events and related granitoids in Wangxianling-Hehuaping area,Nanling Range,South China//12th SGA Biennial Meeting:Mineral Deposit Research for a High-Tech World,3:1343-1346.
Zhou Z M,Ma C Q,Xie C F,Wang L X,Liu Y Y and Liu W.2016.Genesis of highly fractionated I-type granites from Fengshun complex:Implications to tectonic evolutions of South China.Journal of Earth Science,27(3):444-460.
陈毓川,王登红,徐志刚,黄凡.2014.华南区域成矿和中生代岩浆成矿规律概要.大地构造与成矿学,38(2):219-229.
广东省地质局756大队.1985.广东省陆丰县塌山锡矿床详查报告.
华仁民,陈培荣,张文兰,陆建军.2005.论华南地区中生代3次大规模成矿作用.矿床地质,24(2):99-107.
华仁民,李光来,张文兰,胡东泉,陈培荣,陈卫锋,王旭东.2010.华南钨和锡大规模成矿作用的差异及其原因初探.矿床地质,29(1):9-23.
李海立,肖惠良,范飞鹏,陈乐柱,刘建雄,陈叙涛通.2016.广东潮安飞鹅山钨钼多金属矿床辉钼矿Re-Os同位素定年.地质学报,90(2):231-239
李建超,丘元禧.1990.广东莲花山燕山早期断裂动热变质带的基本特征及形成机制的探讨.长春地质学院学报,20(1):93-106.
刘鹏,程彦博,毛景文,王小雨,姚薇,陈叙涛,曾晓剑.2015.粤东田东钨锡多金属矿床花岗岩锆石U-Pb年龄、Hf同位素特征及其意义.地质学报,89(7):1244-1257.
刘师先.1992.塌山斑岩锡矿床地质特征及成矿机理.地球化学,(2):149-157.
路远发.1997.广东钟丘洋次火山岩型铜矿床蚀变围岩的岩石化学特征.华南地质与矿产,(3):1-6.
满发胜,白玉珍,倪守斌,黎彤.1983.莲花山钨矿床同位素地质学初步研究.矿床地质,4(1):35-42.
毛景文,谢桂青,郭春丽,袁顺达,程彦博,陈毓川.2008.华南地区中生代主要金属矿床时空分布规律和成矿环境.高校地质学报,14(4):510-526.
戚建中,黄宾.1988.粤东长埔一西岭地区锡矿断裂岩浆控制因素及成矿模式.中国地质科学院南京矿产地质研究所所刊,9(4):76-94.
丘元禧,丘津松,李建超,钟宏平.1991.广东莲花山断裂带中、新生代多期复合变形变质带的基本特征及其形成机制的探讨.中国地质科学院地质力学研究所所刊,14:93-106
丘增旺,王核,汪礼明,卜安,李莎莎,闫庆贺,暮生禄,李沛,魏小鹏.2016.广东长埔锡多金属矿床石英斑岩锆石U-Pb年代学、Hf同位素组成及其地质意义.地球化学,45(4):374-386.
沈渭洲,凌洪飞.1994.岩背和塌山含锡花岗斑岩的同位素地球化学特征和物质来源.地球学报(1-2):117-123.
涂湘林,张红,邓文峰,凌明星,梁华英,刘颖,孙卫东.2011.RESOlution激光剥蚀系统在微量元素原位微区分析中的应用.地球化学,40(1):83-98.
王德滋,陈绍海,刘昌实,沈渭洲,楚雪君.1995.粤东塌山含锡花岗斑岩原生铝质矿物特征和成因.矿物学报,15(3):249-253.
王小雨.粤东新寮岽铜多金属矿床地质特征及成因初步研究.2015.北京:中国地质大学(北京)硕士学位论文:1-88.
王志强,陈斌,马星华.2014.南岭芙蓉锡矿田锡石原位LA-ICP-MS U-Pb年代学及地球化学研究:对成矿流体来源和演化的意义.科学通报,59(25):2505-2519.
吴福元,李献华,郑永飞,高山.2007.Lu-Hf同位素体系及其岩石学应用.岩石学报,23(2):185-220.
吴淦国,张达,彭润民,吴建设,高天钧,陈柏林等.2004.东南沿海成矿带矿床形成的时间演化规律研究.地学前缘,11(1):237-247.
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589-1604.
徐晓春,岳书仓.1994a.粤东地区中生代火山岩与侵入岩的成因关系及成因类型.合肥工业大学学报(自然科学版),17(4):184-192.
徐晓春,岳书仓.1994b.粤东地区锡多金属矿床的成矿年龄和矿床成因//中国矿物岩石地球化学研究新进展.兰州:兰州大学出版社:347-348.
徐晓春,岳书仓.1996.粤东地区中生代岩浆作用的大地构造背景及构造-岩浆演化.合肥工业大学学报(自然科学版),19(1):127-134.
徐晓春,岳书仓.1999a.粤东锡(钨、铜)多金属矿床的成矿物质来源和成矿作用.地质科学,34(1):81-92.
徐晓春,岳书仓.1999b.粤东中生代花岗质火山-侵入杂岩成因的Nd同位素制约.合肥工业大学学报(自然科学版),22(3):3-6.
徐晓春,岳书仓.1999c.粤东中生代火山-侵入杂岩的地壳深熔成因--Pb-Nd-Sr多元同位素体系制约.地质论评,45(S1):829-835.
岳书仓,雷新勇,龚昌瑞,徐晓春.1989.粤东花岗岩及锡、钨矿床的地球化学研究.中国地质科学院南京地质矿产研究所所刊,10(1):27-41.
邹和平,王建华,丘元禧.2000.广东南澳和莲花山韧性剪切带40Ar/39Ar年龄及其地质意义.地球学报,21(4):356-364.
Amelin Y,Lee D C,Halliday A N,Pidgeon R T.1999.Nature of the Earth’s earliest crust from hafnium isotopes in single detrital zircons.Nature,399(6733):252-255.
Belousova E A,Griffin W L,Suzanne Y,O’Reilly and Fisher N I.2002.Igneous zircon:Trace element composition as an indicator of source rock type.Contributions to Mineralogy and Petrology,143(5):602-622.
Black L P,Kamo S L,Allen C M,Aleinikoff J N,Davis D W,Korsch R J and Foudoulis C.2003.TEMORA 1:A new zircon standard for Phanerozoic U-Pb geochronology.Chemical Geology,200(1):155-170.
Blichert-Toft J and Albarede F.1997.The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle crust system.Earth and Planetary Science Letters,148(1-2):243-258.
Chen X C,Hu R Z,Bi X W,Li H M,Lan J B,Zhao C H and Zhu J J.2014.Cassiterite LA-(MC)ICP-MS U/Pb and muscovite 40Ar/39Ar dating of tin deposits in the Tengchong-Lianghe tin district,NW Yunnan,China.Mineralium Deposita,49(7):843-860.
Chu N C,Taylor R N,Chavagnac V,Nesbitt R W,Boella RM,Milton J A,German C,Bayon G and Burton K.2002.Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry:An evaluation of isobaric interference corrections.Journal of Analytical Atomic Spectrometry,17(12):1567-1574.
Griffin W L,Wang X,Jackson S E,Pearson N J and O’Reilly S Y.2002.Zircon geochemistry and magma mixing,SE China:In-situ analysis of Hf isotopes,Tonglu and Pingtan igneous complexes.Lithos,61(3-4):237-269.
Gulson B L and Jones M T.1992.Cassiterite-potential for direct dating of mineral-deposits and a precise age for the Bushveld complex granites.Geology,20(4):355-358.
Guo F,Fan W M,Li C W,Zhao L,Li H X and Yang J H.2012.Multi-stage crust-mantle interaction in SE China:Temporal,thermal and compositional constraints from the Mesozoic felsic volcanic rocks in eastern GuangdongFujian provinces.Lithos,150:62-84.
Hu R Z and Zhou M F.2012.Multiple Mesozoic mineralization events in South China-an introduction to the thematic issue.Mineralium Deposita,47(6):579-588.
Jiang S Y,Yu J M and Lu J J.2004.Trace and rare-earth element geochemistry in tourmaline and cassiterite from the Yunlong tin deposit,Yunan,China:Implication for migmatitic-hydrothermal fluid evolution and ore genesis.Chemical Geology,209:193-213
Li C Y,Zhang R Q,Ding X,Ling M X,Fan W M and Sun WD.2015.Dating cassiterite using laser ablation ICP-MS.Ore Geology Reviews,72:313-322.
Li X,Long W,Li Q,Liu Y,Zheng Y,Yang Y,Chamberlain KR,Wan D,Guo C and Wang X.2010.Penglai zircon megacrysts:A potential new working reference material for microbeam determination of Hf-O isotopes and U-Pb age.Geostandards and Geoanalytical Research,34(2):117-134.
Liu Y P,Li Z X,Li H M,Guo L G,Xu W,Ye L,Li C Y and Pi D H.2007.U-Pb geochronology of cassiterite and zircon from the Dulong Sn-Zn deposit:Evidence for Cretaceous large-scale granitic magmatism and mineralization events in southeastern Yunnan province,China.Acta Petrological Sinaca,23(5):967-976.
Liu Y S,Hu Z C,Gao S,Günther D,Xu J,Gao C G and Chen H H.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43.
Ludwig,K.R.,2003.User’s Manual for Isoplot 3.00:AGeochronological Toolkit for Microsoft Excel.Berkeley:Berkeley Geochronology Center:1-70.
Ma N,Deng J,Wang Q F,Wang C M,Zhang J and Li GJ.2013.Geochronology of the Dasongpo tin deposit,Yunnan Province:Evidence from zircon LA-ICP-MSU-Pb ages and cassiterite LA-MC-ICP-MS U-Pb age.Acta Petrological Sinaca,29(4),1223-1235.
Mao J W,Cheng Y B,Chen M H and Pirajno F.2013.Major types and time-space distribution of Mesozoic ore deposits in South China and their geodynamic settings.Mineralium Deposita,48(3):267-294.
Mao J W,Pirajno F and Cook N.2011.Mesozoic metallogeny in East China and corresponding geodynamic settingsAn introduction to the special issue.Ore Geology Reviews,43(1):1-7.
Plimer I R,Lu J and Kleeman J D.1991.Trace and rare earth elements in cassiterite-sources of components for the tin deposits of the Mole Granite,Australia.Mineralium Deposita,26:267-274.
Qiu Z W,Li S S,Yan Q H,Wang H,Wei X P,Li P and Bu A.2017a.Late Jurassic Sn metallogeny in eastern Guangdong,SE China coast:Evidence from geochronology,geochemistry and Sr-Nd-Hf-S isotopes of the Dadaoshan Sn deposit.Ore Geology Reviews,83:63-83.
Qiu Z W,Yan Q H,Li S S,Wang H,Tong L X,Zhang R Q,Wei X P,Li P,Wang L M,Bu A and Yan L M.2017b.Highly fractionated Early Cretaceous I-type granites and related Sn polymetallic mineralization in the Jinkeng deposit,eastern Guangdong,SE China:Constraints from geochronology,geochemistry,and Hf isotopes.Ore Geology Reviews,88:718-738.
Rubatto D and Gebauer D.2000.Use of cathodoluminescence for U-Pb zircon dating by ion microprobe:Some examples from the Western Alps//Pagel M,Barbin V,Blanc P and Ohnenstetter D.Cathodoluminescence in Geosciences.Springer Berlin Heidelberg:373-400.
Scherer E,Munker C and Mezger K.2001.Calibration of the lutetium-hafnium clock.Science,293:683-687.
Wang X J,Liu Y P,Miao Y L,Bao T,Ye L and Zhang Q.2014.In-situ LA-MC-ICP-MS cassiterite U-Pb dating of Dulong Sn-Zn polymetallic deposit and its signifycance.Acta Petrologica Sinica,30(3):867-876.
Wu F Y,Yang Y H,Xie L W,Yang J H and Xu P.2006.Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology.Chemical Geology,234(1-2):105-126.
Xie L W,Yin Q Z,Yang J H,Wu F Y and Yang Y H.2013.A tin-mineralized topaz rhyolite dike with coeval topaz granite enclaves at Qiguling in the Qitianling tin district,southern China.Lithos,170:252-268.
Yan Q H,Li S S,Qiu,Z W,Wang H,Wei X P,Dong R and Zhang X Y.2017.Geochronology,geochemistry and Sr-Nd-Hf-S-Pb isotopes of the early cretaceous Taoxihu Sn deposit and related granitoids,SE China.Ore Geology Reviews,89:350-368.
Yan Q H,Qi Z W,Wang H,Wang M,Wei X P,Li P,Zhang RQ,Li C Y and Liu J P.2016.Age of the Dahongliutan rare metal pegmatite deposit,West Kunlun,Xinjiang(NWChina):Constraints from LA-ICP-MS U-Pb dating of columbite-(Fe)and cassiterite.Ore Geology Reviews,http://dx.doi.org/10.1016/j.oregeorev.2016.11.010
Yan Q H,Wang H,Qiu Z W,Wei X P,Li P,Dong R and Zhou K L.2018.Origin of Early Cretaceous A-type granite and related Sn mineralization in the Sanjiaowo deposit,eastern Guangdong,SE China and its tectonic implication.Ore Geology Reviews,93:60-80.
Yuan S D,Peng J T,Hu R Z,Li H M,Shen N P and Zhang DL.2008.A precise U-Pb age on cassiterite from the Xianghualing tin-polymetallic deposit,Hunan,South China.Mineralium Deposita,43:375-382.
Yuan S D,Peng J T,Hu R Z,Li H M,Shen N P and Zhang DL.2011.In situ LA-MC-ICP-MS and ID-TIMS U-Pb geochronology of cassiterite in the giant Furong tin deposit,Hunanb Province,South China:New constraints on the timing of tin-polymetallic mineralization.Ore Geology Reviews,43(1):235-242.
Zhang D L,Peng J T,Coulson I M,Hou L H and Li S J.2014.Cassiterite U-Pb and muscovite 40Ar-39Ar age constraints on the timing of mineralization in the Xuebaoding Sn-W-Be deposit,western China.Ore Geology Reviews,62:315-322.
Zhang R Q,Lu J J,Wang R C,Lu X C,Guo J C,Li F C,Lehmann B,Yao Y and Guo W M.2013.Contrasting Wand Sn mineralization events and related granitoids in Wangxianling-Hehuaping area,Nanling Range,South China//12th SGA Biennial Meeting:Mineral Deposit Research for a High-Tech World,3:1343-1346.
Zhou Z M,Ma C Q,Xie C F,Wang L X,Liu Y Y and Liu W.2016.Genesis of highly fractionated I-type granites from Fengshun complex:Implications to tectonic evolutions of South China.Journal of Earth Science,27(3):444-460.