东天山黄山南镁铁-超镁铁岩体的岩浆演化过程:矿物学、Sr-Nd同位素特征的指示
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摘要
黄山南镁铁-超镁铁质岩体位于东天山造山带觉罗塔格构造带内,属于土墩-黄山-图拉尔根镁铁-超镁铁质岩带。本文在前人研究的基础上,从橄榄石、辉石矿物学组成和全岩Sr、Nd同位素等方面对黄山南岩体进行了分析研究,并与黄山、黄山东、香山等典型含矿岩体作了对比,旨在进一步查明黄山南岩体的岩浆源区和母岩浆性质及其岩浆演化过程。Sr-Nd同位素特征表明黄山南岩体来自一个弱亏损的地幔源区,相较黄山、黄山东、香山等岩体的源区具有更加富集的特征。黄山南岩体中的橄榄石属于贵橄榄石,斜方辉石主要为古铜辉石,少数为紫苏辉石,单斜辉石主要为顽透辉石、普通辉石和少数的透辉石。单斜辉石和橄榄石的成分特征表明形成黄山南岩体的母岩浆为演化程度较低的拉斑玄武质岩浆,且母岩浆成分具有高Mg、高Ni的特点。计算得到黄山南岩体母岩浆的Fe O~T=13.20%、MgO=16.96%、Ni=377.2×10~(-6),且母岩浆在结晶分异过程中没有经历充分的硫化物熔离作用,这也是造成母岩浆中Ni含量较高以及岩体含矿性较差的主要因素。
The Huangshannan mafic-ultramafic intrusion,located in the Jueluotage tectonic zone,East Tianshan orogenic belt,belongs to the Tudun-Huangshan-Tulaergen mafic-ultramafic rock belt.Based on previous research work,the mineral compositions of olivines and pyroxenes of this intrusion,as well as its whole rock Sr-Nd isotopic characteristics were studied in this paper.Further more,by comparison with typical intrusions in the same region,such as the Huangshan,the Huangshandong and the Xiangshan,we try to find its magma source,and to detect the properties and the evolutionary process of its parental magma.The results of Sr-Nd isotopic characteristics of the Huangshannan intrusion indicate that its source comes from a slightly depleted mantle,which is a more enriched mantle source compared with those for the Huangshan,the Huangshandong and the Xiangshan intrusions.All of the olivines from the Huangshannan intrusion are chrysolite.The orthopyroxenes are mainly composed of broncite,with small amount of amblystegite.The clinopyroxenes mainly consist of augite and diopside.The compositions of clinopyroxene and olivine indicate that the parental magma of the Huangshannan intrusion is tholeiitic basalt magma with a low evolution degree,with High Mg and Ni contents.The calculated contents of the parental magma of the Huangshannan intrusion is as follows:Fe O~T=13.20%,MgO=16.96%,Ni=377.2×10~(-6).We also realize that the parental magma doesn’t experience a sufficient sulfide segregation process,which dominantly lead to the high Ni content in its parental magma and poor metallogenetic potentiality of the Huangshannan intrusion.
The Huangshannan mafic-ultramafic intrusion,located in the Jueluotage tectonic zone,East Tianshan orogenic belt,belongs to the Tudun-Huangshan-Tulaergen mafic-ultramafic rock belt.Based on previous research work,the mineral compositions of olivines and pyroxenes of this intrusion,as well as its whole rock Sr-Nd isotopic characteristics were studied in this paper.Further more,by comparison with typical intrusions in the same region,such as the Huangshan,the Huangshandong and the Xiangshan,we try to find its magma source,and to detect the properties and the evolutionary process of its parental magma.The results of Sr-Nd isotopic characteristics of the Huangshannan intrusion indicate that its source comes from a slightly depleted mantle,which is a more enriched mantle source compared with those for the Huangshan,the Huangshandong and the Xiangshan intrusions.All of the olivines from the Huangshannan intrusion are chrysolite.The orthopyroxenes are mainly composed of broncite,with small amount of amblystegite.The clinopyroxenes mainly consist of augite and diopside.The compositions of clinopyroxene and olivine indicate that the parental magma of the Huangshannan intrusion is tholeiitic basalt magma with a low evolution degree,with High Mg and Ni contents.The calculated contents of the parental magma of the Huangshannan intrusion is as follows:Fe O~T=13.20%,MgO=16.96%,Ni=377.2×10~(-6).We also realize that the parental magma doesn’t experience a sufficient sulfide segregation process,which dominantly lead to the high Ni content in its parental magma and poor metallogenetic potentiality of the Huangshannan intrusion.
引文
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Morimoto N.1988.Nomenclature of pyroxenes.Mineralogy and Petrology,39(1):55-76
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Qin KZ,Su BS,Sakyi PA,Tang DM,Li XH,Sun H,Xiao QH and Liu PP.2011.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(NWChina):Constraints on a ca.280Ma mantle PLUME.American Journal of Science,311(3):237-260
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Tang DM,Qin KZ,Sun H,Su BX,Xiao QH,Cheng SL and Li J.2009.Lithological,chromological and geochemical characteristics of Tianyu Cu-Ni deposit:Constrainsts on source and gensis of maficultramafic intrusions in eastern Xinjiang.Acta Petrologica Sinica,25(4):817-831(in Chinese with English abstract)
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Wang BL,Li WY,Zhang ZW,Wang YL,You MX,Qian B and Zhang ZB.2017.Petrological and mineralogical characteristics of the Xiangshanzhong mafic-ultramafic intrusion in eastern Tianshan Mountains:Constrains on rock-forming and ore-forming processes.Geology in China,44(6):1207-1233(in Chinese with English abstract)
Wang YL,Zhang ZW,Zhang JW,You MX,Li K and Wang BL.2016.Mineralogy and Sr-Nd isotope characteristics of Baixintan Ni-Cu deposit in Eastern Tianshan Mountains,Xinjiang,and mineralization process.Acta Geologica Sinica,90(10):2747-2758(in Chinese with English abstract)
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Deng YF,Song XY,Zhou TF,Yuan F,Chen LM and Zheng WQ.2012.Correlations between Fo number and Ni content of olivine of the Huangshandong intrusion,eastern Tianshan,Xinjiang,and the genetic significances.Acta Petrologica Sinica,28(7):2224-2234(in Chinese with English abstract)
Deng YF,Song XY,Chen LM,Zhou TF,Pirajno F,Yuan F,Xie Wand Zhang DY.2014.Geochemistry of the Huangshandong Ni-Cu deposit in northwestern China:Implications for the formation of magmatic sulfide mineralization in orogenic belts.Ore Geology Reviews,56:181-198
Fan YZ,Wang Y,Chen DL,Wang ZX and Xia MZ.2014.Study on the petrogenesis and mineralogy of Huangshannan basic-ultrabasic intrusion in East Tianshan,Xinjiang.Xinjiang Geology,32(3):310-315(in Chinese with English abstract)
Han BF,Ji JQ,Song B,Chen LH and Li ZH.2004.SHRIMP zircon U-Pb ages of Kalatongke No.1 and Huangshandong Cu-Ni-bearing mafic-ultramafic complexes,North Xinjiang,and geological implications.Chinese Science Bulletin,49(22):2424-2429
Leterrier J,Maury RC,Thonon P,Girard D and Marchal M.1982.Clinopyroxene composition as a method of identification of the magmatic affinities of paleo-volcanic series.Earth and Planetary Science Letters,59(1):139-154
Li CS,Ripley EM and Naldrett AJ.2003.Compositional variations of olivine and sulfur isotopes in the Noril’sk and Talnakh intrusions,Siberia:Implications for ore-forming processes in dynamic magma conduits.Economic Geology,98(1):69-86
Li CS,Naldrett AJ and Ripley EM.2007.Controls on the Fo and Ni contents of olivine in sulfide-bearing mafic/ultramafic intrusions:Principles,modeling,and examples from Voisey’s Bay.Earth Science Frontiers,14(5):177-183
Li SB,Hu RZ,Song XY,Chen LM and Shen NP.2008.Sulfide separation control in Ni content of olivine in bearing-ore intrusion of magma deposit:An example from Jinchuan intrusion.Bulletin of Mineralogy,Petrology and Geochemistry,27(2):146-152(in Chinese with English abstract)
Mao YJ.2014.Petrogenesis and ore genesis of the multi-stage maficultramafic intrusions in the Huangshannan Ni-Cu ore camp,Eastern Tianshan,southern Central Asian Orogenic Belt.Ph.D.Dissertation.Beijing:University of Chinese Academy of Sciences,1-177(in Chinese)
Mao YJ,Qin KZ,Tang DM,Feng HY and Xue SC.2016.Crustal contamination and sulfide immiscibility history of the Permian Huangshannan magmatic Ni-Cu sulfide deposit,East Tianshan,NWChina.Journal of Asian Earth Sciences,129:22-37
Morimoto N.1988.Nomenclature of pyroxenes.Mineralogy and Petrology,39(1):55-76
Naldrett AJ.1989.Magmatic Sulfide Deposits:Geology,Geochemistry and Exploration.Oxford:Oxford University Press
Naldrett AJ.1999.World-class Ni-Cu-PGE deposits:Key factors in their genesis.Mineralium Deposita,34(3):227-240
Qin KZ,Su BS,Sakyi PA,Tang DM,Li XH,Sun H,Xiao QH and Liu PP.2011.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(NWChina):Constraints on a ca.280Ma mantle PLUME.American Journal of Science,311(3):237-260
Qiu JX and Liao QA.1996.Petrogenesis and Cpx mineral chemistry of Cenozoic basalts from Zhejiang and Fujian of eastern China.Volcanology&Mineral Resources,17(1-2):16-25(in Chinese with English abstract)
San JZ,Qin KZ,Tang ZL,Tang DM,Su BX,Sun H,Xiao QH and Liu PP.2010.Precise zircon U-Pb age dating of two mafic-ultramafic complexes at Tulargen large Cu-Ni district and its geological implications.Acta Petrologica Sinica,26(10):3027-3035(in Chinese with English abstract)
Sun T,Wang DH,Qian ZZ,Fu Y,Chen ZH and Lou DB.2014.Summary of metallogenic regularity for the nickel deposits,China.Acta Geologica Sinica,88(12):2227-2251(in Chinese with English abstract)
Tang DM,Qin KZ,Sun H,Su BX,Xiao QH,Cheng SL and Li J.2009.Lithological,chromological and geochemical characteristics of Tianyu Cu-Ni deposit:Constrainsts on source and gensis of maficultramafic intrusions in eastern Xinjiang.Acta Petrologica Sinica,25(4):817-831(in Chinese with English abstract)
Tang DM,Qin KZ,Su BX,Sakyi PA,Liu YS,Mao Q,Santosh M and Ma YG.2013.Magma source and tectonics of the Xiangshanzhong mafic-ultramafic intrusion in the Central Asian Orogenic Belt,NWChina,traced from geochemical and isotopic signatures.Lithos,170-171:144-163
Wang BL,Li WY,Zhang ZW,Wang YL,You MX,Qian B and Zhang ZB.2017.Petrological and mineralogical characteristics of the Xiangshanzhong mafic-ultramafic intrusion in eastern Tianshan Mountains:Constrains on rock-forming and ore-forming processes.Geology in China,44(6):1207-1233(in Chinese with English abstract)
Wang YL,Zhang ZW,Zhang JW,You MX,Li K and Wang BL.2016.Mineralogy and Sr-Nd isotope characteristics of Baixintan Ni-Cu deposit in Eastern Tianshan Mountains,Xinjiang,and mineralization process.Acta Geologica Sinica,90(10):2747-2758(in Chinese with English abstract)
Xia MZ,Jiang CY,Qian ZZ,Xia ZD,Wang BY and Sun T.2010.Geochemistry and petrogenesis of Huangshandong intrusion,East Tianshan,Xinjiang.Acta Petrologica Sinica,26(8):2413-2430(in Chinese with English abstract)
Xu G,Tang ZL,Wang YL,Yan HQ,Jiao JG and Wang JZ.2012.Features and genetic significance of olivine from Heishan magmatic sulfide ore-bearing intrusion in Beishan area,Gansu Province.Mineral Deposits,31(5):1075-1086(in Chinese with English abstract)
Xu MX and Li ZQ.1992.Discussion of petrographic characteristics and origin of Huangshannan ore-bearing mafic-ultramific complex,in Hami,Xinjiang.Journal of Chengdu College of Geology,19(1):77-84(in Chinese with English abstract)
You MX,Zhang ZW,Wang YL,Qian B and Zhang JW.2017.Zircon U-Pb age and the magma evolution process of the Huangshannan mafic-ultramafic intrusion in the East Tianshan Mountains.Geology and Exploration,53(5):903-914(in Chinese with English abstract)
Zhang LY,Li N and Prelevi c'D.2016.The research status of olivine trace elements in-situ analysis and perspectives of its application.Acta Petrologica Sinica,32(6):1877-1890(in Chinese with English abstract)
Zhang MJ,Li CS,Fu PE,Hu PQ and Ripley EM.2011.The Permian Huangshanxi Cu-Ni deposit in western China:Intrusive-extrusive association,ore genesis,and exploration implications.Mineralium Deposita,46(2):153-170
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