[1]苏 晔,李光来,唐 傲.2020.赣中聚源钨矿区花岗斑岩锆石U-Pb年代学、岩石地球化学和Sr-Nd-Hf同位素特征及成因探讨.大地构造与成矿学,44(5):971-985.doi:10.16539/j.ddgzyckx.2020.05.010
　SU Ye,LI Guanglai,TANG Ao.2020.Zircon U-Pb Age, Petrochemistry, Sr-Nd-Hf Isotopic Features and Genesis of Granite Porphyry from Juyuan Tungsten Deposit in Central Jiangxi Province.Geotectonica et Metallogenia,44(5):971-985.doi:10.16539/j.ddgzyckx.2020.05.010
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赣中聚源钨矿区花岗斑岩锆石U-Pb年代学、岩石地球化学和Sr-Nd-Hf同位素特征及成因探讨
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2020年44卷05期
页码:
971-985
栏目:
岩石大地构造与地球化学
出版日期:
2020-10-20

文章信息/Info

Title:
Zircon U-Pb Age, Petrochemistry, Sr-Nd-Hf Isotopic Features and Genesis of Granite Porphyry from Juyuan Tungsten Deposit in Central Jiangxi Province
文章编号:
1001-1552(2020)05-0971-015
作者:
苏 晔1.2;  李光来1*;  唐 傲1;  李成祥1;  韦星林3;  尹晓燕1
1.东华理工大学 放射性地质与勘探技术国防重点学科实验室, 江西 南昌 330013; 2.甘肃省地质环境监测院, 甘肃 兰州 730050; 3.江西省核工业地质局, 江西 南昌 330046
Author(s):
SU Ye1.2;  LI Guanglai1*;  TANG Ao1;  LI Chengxiang1;  WEI Xinglin3 and YIN Xiaoyan1
1. Fundamental Science on Radioactive Geology and Exploration Technology Laboratory, East China University of Technology, Nanchang 330046, Jiangxi, China; 2. Environment Monitoring Institute of Gansu Province, Lanzhou 730050, Gansu, China; 3. Jinagxi Nuclear Industry Geological Bureau, Nanchang 330046, Jiangxi, China
关键词:
锆石U-Pb定年;  岩石地球化学;  Sr-Nd-Hf同位素;  花岗斑岩;  赣中
Keywords:
zircon U-Pb age;  petrological geochemistry;  Sr-Nd-Hf isotopic;  granite porphyry;  central Jiangxi province
分类号:
P581.121; P597.3
DOI:
10.16539/j.ddgzyckx.2020.05.010
文献标志码:
A
摘要:
聚源钨矿是赣中地区的一个大型石英脉型白钨矿床。通过对与矿床密切相关的花岗斑岩开展锆石U-Pb年代学、岩石地球化学以及Sr-Nd-Hf同位素研究, 结果表明, 其形成年龄为152.4±1.0 Ma。花岗斑岩具有高硅(SiO2=75.08%~ 76.11%), 富碱(K2O+Na2O=7.82%~8.70%), 富钾(K2O=4.57%~5.39%), 强过铝质(A/CNK=1.05~1.20, 均值>1.1)的特征; 富集Rb、Th、U、K、Sm等元素, 强烈亏损Ba、Sr、P、Ti、Zr和Eu等元素, 与S型花岗岩特征类似; 轻稀土元素富集, 重稀土元素亏损((La/Yb)N=14.07~15.89), Eu强烈亏损(δEu=0.04~0.11)。岩石的ISr值介于0.709702~0.717566之间, 平均为0.714717, εNd(t)值为?8.8~?8.1, 锆石εHf(t)值在?11.9~?9.3之间, 两阶段Nd模式年龄和两阶段Hf模式年龄分别为1.60~1.66 Ga、1.78~1.95 Ga, 这些特征表明聚源花岗斑岩岩浆源区主要为古元古代地壳物质。岩体形成与燕山早期华南地区岩石圈伸展-减薄有关。
Abstract:
The Juyuan tungsten deposit, located in the central Jiangxi province, is a large quartz vein type scheelite deposit. Geochronological, geochemical and Sr-Nd-Hf isotope geochemical investigations were carried out on the Juyuan granite porphyry which is believed to be closely related to the formation of the Juyuan tungsten deposit. LA-ICP-MS zircon U-Pb dating results showed that the Juyuan granite porphyry was formed at 152.4±1.0 Ma. The granite porphyry is a S-type granite. It has high contents of SiO2 (SiO2=75.08%-76.11%), Alk (K2O+Na2O=7.82%-8.70%), K2O (K2O=4.57%-5.39%) and high ratios of A/CNK (A/CNK=1.05-1.20, mean value>1.1). The granite porphyry is enriched in Rb, U, Th, K, Sm and a strong negative anomalies of P, Ti, Zr, Ba, Sr and Eu, which is typical for S type granite. The granite porphyry is also enriched in LREE and depleted in HREE, and has an obvious negative Eu anomalies (δEu=0.04-0.11). The granite porphyry has initial 87Sr/86Sr values varying in range of 0.709702 to 0.717566, with an average of 0.714717, εNd(t) values of ?8.8 to ?8.1, and zircon εHf(t) values of ?11.9 to ?9.3, Nd and Hf model ages of 1.60-1.66 Ga and 1.78-1.95 Ga, these characteristics indicate that the granite porphyry was originated from partial melting of Paleoproterozoic crustal rocks. The granite porphyry is formed in lithospheric extending-thinning environment during the Early Yanshanian in South China.

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备注/Memo

备注/Memo:
收稿日期: 2019-01-01; 改回日期: 2019-06-15
项目资助: 国家自然科学基金项目(41862004、41972071)资助。
第一作者简介: 苏晔(1988-), 男, 硕士研究生, 地质工程专业。Email: sjj19881221@126.com
通信作者: 李光来(1983-), 男, 副教授, 硕士生导师, 从事花岗岩与成矿作用研究。Email: liguanglai@ecit.cn
更新日期/Last Update: 2020-10-20