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引用本文:周 洁1,2 姜耀辉1 曾 勇2 葛伟亚2. 江南造山带东段旌德岩体锆石LA-ICPMS年龄和Nd-Sr-Hf同位素地球化学[J]. 中国地质, 2013, 40(5): 1379-1391.
ZHOU Jie1,2, JIANG Yao-hui1, ZENG Yong2, GE Wei-ya2. Zircon U-Pb age and Sr, Nd, Hf isotope geochemistry of Jingde pluton in eastern Jiangnan orogen, South China[J]. Geology in China, 2013, 40(5): 1379-1391(in Chinese with English abstract).
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江南造山带东段旌德岩体锆石LA-ICPMS年龄和Nd-Sr-Hf同位素地球化学
周 洁1,2 姜耀辉1 曾 勇2 葛伟亚21,2
1.南京大学内生金属矿床成矿机制研究国家重点实验室,地球科学与工程学院,江苏 南京 210093;2.中国地质调查局南京地质调查中心,江苏 南京210016
摘要:
提要:旌德花岗质杂岩体位于安徽南部,由花岗闪长岩和二长花岗岩组成。本研究得到岩体中锆石U-Pb年龄为(141.0±1.0) Ma,认为该年龄代表岩体的侵位年龄。岩体全岩主量元素特征显示出中偏酸性 (SiO2=66.01%~70.87%),富Al (Al2O3=14.91%~16.24%),富碱 (alk = 6.64%~8.01%),K2O/Na2O变化范围在0.78~1.04,镁、铁含量较低,MgO:0.68%~1.06%,TFe2O3 (2.0%~3.34%),以及低磷 (P2O5 =0.10%~0.14%)的特点;微量元素主要富集Sr (189×10-6~452×10-6),贫Nb、Ta、P、Ti、Y、Yb,高Sr/Y比值 (23~66)和 (La/Yb)N (13~58),Eu有轻微的负异常到弱的正异常 (δEu=0.81~1.18)。旌德岩体的地球化学特征与中国东部中生代埃达克质岩相似。ISr=0.7096~0.7101, εNd(t)=-6.28~-7.32,εHf(t)值变化于-6.5~-1.1,两阶段模式年龄 tDM2=1.4~1.5 Ga。较年轻的Nd同位素模式年龄、较高的εNd(t)值和εHf(t)值,以及岩体中发育有岩浆混合成因的暗色包体,指示源区可能有地幔物质的贡献。幔源岩浆底侵使下地壳发生部分熔融,并发生了岩浆混合作用,形成了旌德岩体。
关键词:  旌德岩体  岩石地球化学  锆石U-Pb年龄  Sr-Nd-Hf同位素
DOI:
分类号:
基金项目:国家自然科学青年基金项目(41002017) 资助。
Zircon U-Pb age and Sr, Nd, Hf isotope geochemistry of Jingde pluton in eastern Jiangnan orogen, South China
ZHOU Jie1,2, JIANG Yao-hui1, ZENG Yong2, GE Wei-ya21,2
1. State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, Jiangsu, China;2. Nanjing Center of China Geological Survey, Nanjing 210016, Jiangsu, China
Abstract:
Abstract:Jingde pluton is one of the Mesozoic plutons in eastern Jiangnan orogen of northeast Yangzte Block. New LA-ICPMS zircon U-Pb dating for one granodiorite yielded an emplacement age of (141.0±1.0) Ma. The pluton is composed of monzogranite and granodiorite. New petrographical and petrochemical data show that the pluton is intermediate-somewhat acid (SiO2=66.01%~70.87%), and has high content of Al2O3 (Al2O3=14.91%~16.24%) and rich alkali (K2O+Na2O = 6.64%~8.01% ), with K2O/Na2O value ranging from 0.78 to 1.04. The pluton has relatively low content of MgO, TFe2O3 and P2O5 (MgO = 0.68%~1.06%, TFe2O3=2.0%~3.34%, P2O5 = 0.10%~0.14% ). As for trace elements, the pluton is enriched in Sr (189×10-6~452×10-6) with high Sr/Y ratios (23~66) and also enriched in light rare earth elements (LREE) ((La/Yb)N = 13 ~ 58) , but somewhat depleted in Nb, Ta, P, Ti, Y, Yb, with slightly negligible to positive Eu anomalies (δEu=0.81~1.18), similar to the geochemical characteristics of Mesozoic adakitoid in eastern China. Jingde pluton has relatively high Nd isotopes (εNd(t)=-6.28~-7.32), high εHf (t) values (-6.5~-1.1) and younger tDM2 model ages (1.4~1.5Ga), with mafic microgranular enclaves (MMEs), suggesting the importance of mantle material in the magma source. The mafic magmas ascended and heated the lower crust, triggering the partial melting of the lower crust to form the Jingde pluton, with the input of mantle-derived materials.
Key words:  Jingde pluton  geochemistry  zircon U-Pb age  Sr, Nd, Hf isotopes