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浙江中部芙蓉山花岗斑岩及包体岩石地球化学研究
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引用本文:杜秀玲,汪方跃,闫海洋,顾海欧,孙贺,葛粲.2021.浙江中部芙蓉山花岗斑岩及包体岩石地球化学研究[J].地质论评,67(5):67060002,[DOI]:.
DU Xiuling,WANG Fangyue,YAN Haiyang,GU Haiou,SUN He,GE Can.2021.Geochemistry of Furongshan Granitic Porphyry and Mafic Microgranular Enclaves in Central Zhejiang Province[J].Geological Review,67(5):67060002.
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作者单位E-mail
杜秀玲 1)合肥工业大学资源与环境工程学院合肥230009
2)合肥工业大学矿床成因与勘查技术研究中心合肥230009 
duxiuling0202@163.com 
汪方跃 1)合肥工业大学资源与环境工程学院合肥230009
2)合肥工业大学矿床成因与勘查技术研究中心合肥230009 
fywang@hfut.edu.cn 
闫海洋 3)中国科学院壳幔物质与环境重点实验室中国科学技术大学地球和空间科学学院合肥230026  
顾海欧 1)合肥工业大学资源与环境工程学院合肥230009
2)合肥工业大学矿床成因与勘查技术研究中心合肥230009 
 
孙贺 1)合肥工业大学资源与环境工程学院合肥230009
2)合肥工业大学矿床成因与勘查技术研究中心合肥230009 
 
葛粲 1)合肥工业大学资源与环境工程学院合肥230009
2)合肥工业大学矿床成因与勘查技术研究中心合肥230009 
 
基金项目:国家重点研发计划“深地资源勘查开采”重点专项(2016YFC0600404)、 国家自然科学基金项目(41873034)
中文摘要:花岗岩的源区、温压条件及与其他岩石的共生组合的研究可以限定其形成构造背景,了解其形成的深部动力学过程。本文对浙江中部中生代芙蓉山花岗斑岩及其暗色包体开展了全岩主微量元素、锆石U-Pb年代学和Hf同位素、Ti温度计和全岩Sr-Nd同位素研究,探讨芙蓉山花岗斑岩的成因类型、源区特征及其与镁铁质包体之间的关系,并进一步限定其构造背景。锆石U-Pb定年结果显示芙蓉山花岗斑岩加权平均年龄为133.6±1.6 Ma (MSWD = 2.1,2σ),镁铁质包体加权平均年龄为130.3±4.2 Ma (MSWD = 5.8,2σ),其成岩年龄基本一致,形成于早白垩世。全岩地球化学表明芙蓉山花岗斑岩属于亚碱性系列,同时具有低的Ga/Al(<2.6),高的Na2O含量(2.75%-4.5%,平均3.78%),较高的全碱含量(Na2O + K2O = 7.93%-8.75%),以及较低的锆石Ti饱和温度特征(631-690℃),这些特征显示芙蓉山花岗斑岩为I型花岗岩,而非A型花岗岩。芙蓉山花岗斑岩中锆石Hf同位素有比较大的范围[εHf(t)=-10.9~-1.1],全岩[n(87Sr)/ n(86Sr)]i = 0.7062-0.7078,相对富集的εNd(t)=-5.6 ~ -4.7值;而包体表现为均一的[n(87Sr)/ n(86Sr)]i=0.7071-0.7079和弱富集的εNd(t)=-3.8 ~-2.8特征。野外及岩相学和元素地球化学特征显示典型的岩浆混合特征。镁铁质包体源区可能来自于俯冲交代地幔,芙蓉山花岗斑岩则形成于古老富钾地壳熔体和交代地幔熔体混合后的结晶分异。混合模型计算表明混合比例为:~80%的地幔端元和~ 20%地壳端元。浙江中部芙蓉山富钾I型花岗斑岩与镁铁质包体共生可能指示其形成于古太平洋板块俯冲后撤初始弱伸展拉张的构造背景。
中文关键词:赣杭构造带  芙蓉山岩体  I型花岗岩  岩浆混合  古太平洋俯冲  洋壳俯冲后撤
 
Geochemistry of Furongshan Granitic Porphyry and Mafic Microgranular Enclaves in Central Zhejiang Province
NameInstitution
DU Xiuling1)School of Resources and Environmental Engineering, Hefei University of Technology,Hefei,230009,China;2)Ore Deposit and Exploration Center (ODEC),Hefei University of Technology,Hefei,230009,China
WANG Fangyue1)School of Resources and Environmental Engineering, Hefei University of Technology,Hefei,230009,China;2)Ore Deposit and Exploration Center (ODEC),Hefei University of Technology,Hefei,230009,China
YAN Haiyang3)Chinese Academy of Sciences (CAS) Key Laboratory of Crust-Mantle Materials and Environments,School of Earth and Space Sciences,University of Science and Technology of China,Hefei,230026,China
GU Haiou1)School of Resources and Environmental Engineering, Hefei University of Technology,Hefei,230009,China;2)Ore Deposit and Exploration Center (ODEC),Hefei University of Technology,Hefei,230009,China
SUN He1)School of Resources and Environmental Engineering, Hefei University of Technology,Hefei,230009,China;2)Ore Deposit and Exploration Center (ODEC),Hefei University of Technology,Hefei,230009,China
GE Can1)School of Resources and Environmental Engineering, Hefei University of Technology,Hefei,230009,China;2)Ore Deposit and Exploration Center (ODEC),Hefei University of Technology,Hefei,230009,China
Abstract:Objectives: By comparing the geochemistry and isotopic compositions of Furongshan granitic porphyry and mafic microgranular enclaves from central Zhejiang province, the genesis of Furongshan granitic porphyry,the characteristic of source area and the relationship between granitic porphyry and mafic microgranular enclaves are able to be explored,through which further constraints of the tectonic setting, and the geodynamic process of the Late Mesozoic crust-mantle magma interaction in the South China Plate could be revealed.Methods: Based on the field work, through the microscope observation,the whole rock chemical analysis,LA ICP-MS zircon U-Pb dating,Ti-thermometer,Sr-Nd isotopic compositions and Hf isotopes of Mesozoic host granitic porphyry and their mafic microgranular enclaves (MMEs) from Furongshan pluton.Results: Zircon U-Pb dating results show that the weighted mean n(206Pb)/ n(238U) age of Furongshan granitic porphyry is 133.6±1.6 Ma (MSWD=2.1,2σ),and the weighted mean n(206Pb)/ n(238U) age of mafic microgranular enclaves is 130.3±4.2 Ma (MSWD=5.8, 2σ). Their diagenetic ages are basically the same and formed in the early Cretaceous.The Furongshan granitic porphyry are?sub-alkaline with low Ga/Al(<2.6)(10000*Ga/Al=2.19-2.48)and high Na2O(2.75-4.5%),enriched in alkalis (Na2O+K2O=7.93-8.75%).And calculated results based on zircon Ti-thermometry indicate a relatively low magmatic temperature(631-690℃).The Furongshan granitic porphyry has a large range of zircon εHf(t) values (-10.9~-1.1) and exhibits initial [n(87Sr)/n(86Sr)]i ratios of 0.7062 to 0.7078 and εNd(t) values of-5.6 to -4.7,the enclaves have relatively uniform initial [n(87Sr)/ n(86Sr)]i ratios of 0.7071 to 0.7079 and εNd(t) values of -3.8 to -2.8.Conclusions: These petrographical and geochemical characteristics of the Furongshan granitic porphyry suggest I-type granitic affinities rather than A-type granitic affinities.Field and petrography and geochemistry characteristics suggesting Furongshan mafic microgranular enclaves and host granitic porphyry were formed by magma mixing. The source of mafic microgranular enclaves may be derived from the subduction metasomatic mantle,and the Furongshan granitic porphyry was formed by the fractional crystallization after the mixing of ancient K-rich crustal melt and metasomatic mantle melt.The modeling results indicate that the hybrid magma may have been formed by~80% basaltic and ~20% felsic melts.The Furongshan K-rich I type granitic porphyry and the enclaves in the central Zhejiang province may indicate that they were formed in the tectonic setting of weak extension at the earlier stage of the roll-back of paleo-Pacific plate subduction. Acknowledgements: This study was supported by the Deep Resources Exploration and Mining,a Special Project in the Framework of National Key R&D Program of China (No.2016YFC0600404) and the National Science Foundation of China (No. 41873034).
keywords:Furongshan  I-type granites  Magma mixing  Paleo-Pacific plate subduction  Oceanic crust subduction and retreat
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