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东昆仑诺木洪地区新元古代眼球状花岗片麻岩锆石U-Pb年龄及Hf同位素特征
引用本文:徐佳丽,周文孝,赵晓成,王波,李海泉,常风,吕新彪.东昆仑诺木洪地区新元古代眼球状花岗片麻岩锆石U-Pb年龄及Hf同位素特征[J].矿产勘查,2020,11(1):1-9.
作者姓名:徐佳丽  周文孝  赵晓成  王波  李海泉  常风  吕新彪
作者单位:中国地质大学武汉环境学院,武汉 430074,中国地质大学武汉地质调查研究院, 武汉 430074,新疆维吾尔自治区地震局,乌鲁木齐 830011,中国地质大学武汉地质调查研究院, 武汉 430074,中国地质大学武汉地质调查研究院, 武汉 430074,中国地质大学武汉地质调查研究院, 武汉 430074,中国地质大学武汉地质调查研究院, 武汉 430074;中国地质大学武汉资源学院,武汉 430074;中国地质大学武汉地质过程与矿产资源国家重点实验室,武汉 430074
基金项目:国家自然科学基金项目(编号:41703024)和中国地质调查局地质矿产调查项目(编号:12120114018001)联合资助。
摘    要:对东昆仑诺木洪地区白沙河岩组眼球状花岗片麻岩中。锆石进行U-Pb测年结果表明,该片麻岩可能形成于921 Ma左右,其中含有的残留锆石核反映其可能来自于中元古代地壳物质的再循环;对锆石Hf同位素测定结果显示其具有正的εHf(t),且位于1100~1500 Ma的平均地壳演化线之间,同样暗示其来自于中元古代古老地壳物质。结合区域上存在同时期的双峰式侵入岩,推测该眼球状花岗片麻岩形成于伸展环境下,地幔上涌引起上覆中元古代的白沙河岩组为代表的表壳岩系发生熔融,并侵入其中,之后再共同经历了后期的角闪岩相变质。

关 键 词:东昆仑  白沙河岩组  眼球状花岗片麻岩  锆石U-PB  HF同位素  地质调查工程
收稿时间:2019/8/7 0:00:00

Zircon U-Pb age and Hf isotopic characteristics of the Neoproterozoic globular granitic gneiss in Nomuhong area, east Kunlun
Affiliation:School of Environmental Studies, China University of Geosciences, Wuhan 430074,Institute of Geological Survey, China University of Geosciences, Wuhan 430074,Xinjiang Earthquake Administration, China Earthquake Administration, Urumqi 830011,Institute of Geological Survey, China University of Geosciences, Wuhan 430074,Institute of Geological Survey, China University of Geosciences, Wuhan 430074,Institute of Geological Survey, China University of Geosciences, Wuhan 430074 and Institute of Geological Survey, China University of Geosciences, Wuhan 430074;Faculty of Earth Resources, China University of Geosciences Wuhan, Wuhan 430074;State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences Wuhan, Wuhan 430074
Abstract:Zircon U-Pb geochronology and zircon Hf isotope study were carried out on the spheroidal granitic gneiss in the Baishahe Formation of the Nomuhong area in east Kunlun. The zircon U-Pb dating results indicate that the gneiss may be formed at around 921 Ma,and the residual zircon core contained therein may reflect the recirculation of the Mesoproterozoic crustal material. The zircon Hf isotope results show that it has a positive εHf(t) and lies between the average crust evolution lines of 1100 ~ 1500 Ma,which also implies that it originated from the Middle Proterozoic ancient crustal material. There are contemporaneous bimodal intrusive rocks in the combined area. It is speculated that the globular granitic gneiss may be formed in the extended environment,and the mantle upwell caused the overlying metamorphic Paleozoic Baishahe Formation as the representative case rock series. Melting occurs and invades it,and then undergoes a later amphibolite facies metamorphism.
Keywords:east Kunlun  Baishahe Formation  globular granitic gneiss  zircon U-Pb  Hf isotope  geological surrey engineering
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