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江西冷水坑矿床含矿花岗斑岩的Sr-Nd及锆石Hf-O同位素研究

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龚雪婧, 曾建辉, 曹殿华. 2019. 江西冷水坑矿床含矿花岗斑岩的Sr-Nd及锆石Hf-O同位素研究[J]. 中国地质, 46(4): 818-831. doi: 10.12029/gc20190412
引用本文: 龚雪婧, 曾建辉, 曹殿华. 2019. 江西冷水坑矿床含矿花岗斑岩的Sr-Nd及锆石Hf-O同位素研究[J]. 中国地质, 46(4): 818-831. doi: 10.12029/gc20190412
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GONG Xuejing, ZENG Jianhui, CAO Dianhua. 2019. Sr-Nd and zircon Hf-O isotopic constraints on the petrogenesis of the orebearing granitic porphyry at Lengshuikeng, Jiangxi Province[J]. Geology in China, 46(4): 818-831. doi: 10.12029/gc20190412
Citation: GONG Xuejing, ZENG Jianhui, CAO Dianhua. 2019. Sr-Nd and zircon Hf-O isotopic constraints on the petrogenesis of the orebearing granitic porphyry at Lengshuikeng, Jiangxi Province[J]. Geology in China, 46(4): 818-831. doi: 10.12029/gc20190412
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江西冷水坑矿床含矿花岗斑岩的Sr-Nd及锆石Hf-O同位素研究

  • 1.

    中国地质科学院, 北京 100037

  • 2.

    中国地质调查局-中国地质科学院地球深部探测中心, 北京 100037

  • 3.

    江西省地质矿产勘查开发局九一二大队, 江西 鹰潭 335000

  • 基金项目:
    中国地质调查局项目（DD20160082，DD20190012）、国家自然科学基金（41802097）及国家重点研发计划“深地资源勘查开采”重点专项（2016YFC0600201）联合资助
详细信息
    作者简介: 龚雪婧, 女, 1988年生, 博士, 助理研究员, 主要从事岩石地球化学及矿床学研究, Email:xuejinggong@cags.ac.cn

  • 中图分类号: P588.13;P597

Sr-Nd and zircon Hf-O isotopic constraints on the petrogenesis of the orebearing granitic porphyry at Lengshuikeng, Jiangxi Province

  • 1.

    Chinese Academy of Geological Sciences, Beijing 100037, China

  • 2.

    SinoProbe Center, Chinese Academy of Geological Sciences and China Geological Survey, Beijing 100037, China

  • 3.

    No. 912 Geological Party of Jiangxi Bureau of Geology and Mineral Exploration and Development, Yingtan 335001, Jiangxi, China

  • Fund Project: Supported jointly by Project of China Geological Survey (No.DD20160082, No.DD20190012), National Natural Science Foundation (No. 41802097), National Key Research and Development Program (No. 2016YFC0600201)
More Information
    Author Bio: GONG Xuejing, female, born in 1988, doctor, assistant professor, engages in research on petrogeochemistry and economic geology; E-mail:xuejinggong@cags.ac.cn .

    摘要

  • 江西冷水坑铅锌矿床是武夷成矿带北段的典型矿床，矿区内含矿花岗斑岩锆石U-Pb年龄为（162.0±2.0）Ma，岩浆分异程度较高，具有高SiO2（69.46%~75.52%）、高K2O（K2O/Na2O>3.22）、强过铝质（ASI=1.20~1.96）的特征。岩体发育较明显的Eu负异常，富集强不相容元素Rb、Th、U，而亏损高场强元素Ba、Sr、Nb、Ta、P、Ti。全岩同位素测试结果显示，冷水坑含矿花岗斑岩具有极高的87Sr/86Sr初始比值（0.74005~0.76518）与低的εNd值（-11.48~-10.78），锆石Hf-O同位素测定值变化范围较小，176Hf/177Hf介于0.282317~0.282460，具有负的εHf（t）值（-12.39~-7.62）和相对较高的δ18O值（7.23‰~8.81‰），指示岩浆主要来自于成熟地壳，可能起源于北武夷地区变质基底，源岩为基底变质岩，这可能与古太平洋板块俯冲形成的挤压背景下的地壳熔融有关。

    The Lengshuikeng lead-zinc deposit in Jiangxi Province is a typical deposit in the northern section of the Wuyi metallogenic belt. The zircon SHRIMP U-Pb age of the ore-bearing granite porphyry in the mining area is (162.0±2.0) Ma. The granite porphyries are highly evolved, with high SiO2 (69.46%~75.52%), high K2O (K2O/Na2O>3.22) and strong peraluminous (ASI=1.20~1.96). The negative Eu anomalies of the rock mass are relatively strong, and enriched in LILE such as Rb, Th, and U, while the HFSE such as Ba, Sr, Nb, Ta, P, and Ti are depleted. In this study, the authors also report Sr-Nd and zircon Hf-O isotopic compositions of the granitic porphyries at Lengshuikeng. The results show that the granitic porphyries have relatively high initial 87Sr/86Sr ratios (0.74005~0.76518) and negative εNd values (-11.48~-10.78) as well as the zircon Hf-O isotope measurement value. The variation range of 176Hf/177Hf values (0.282317~0.282460) is small, with negative εHf(t) values (-12.39~-7.62) and relatively high δ18O values (7.23‰~8.81‰), indicating that the magma mainly came from the mature crust, which may have originated from metamorphic basement of North Wuyi area, and the source rocks were probably the metamorphic basement. The magmatic activity was probably related to the crust melting under the compressive background formed by northwestward subduction of the Paleo-Pacific Plate.

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  • 图 1  冷水坑矿床区域构造简图(a)、冷水坑矿区地质简图（b）及100勘探线剖面图（c）（b, c据江西省地质矿产勘查开发局912地质队，1997）

    Figure 1. 

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    图 2  冷水坑花岗斑岩样品矿物组合特征

    Figure 2. 

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    图 3  冷水坑花岗斑岩锆石阴极发光图像、测试位置（小圆圈代表SHRIMP U-Pb和O同位素分析点，大圆圈代表LA-MCICP-MS Hf同位素分析点）和结果（分析点旁边的数字表示U-Pb年龄和εHf(t)/δ18O值）及SHRIMP锆石U-Pb协和图

    Figure 3. 

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    图 4  岩石类型和系列划分图解

    Figure 4. 

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    图 5  稀土元素球粒陨石标准化配分曲线图（a）和微量元素原始地幔标准化配分曲线图(b)（球粒陨石、原始地幔数据据Sun et al., 1989）

    Figure 5. 

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    图 6  冷水坑花岗斑岩锆石Hf同位素（a）和O同位素（b）组成频数统计图

    Figure 6. 

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    图 7  冷水坑花岗斑岩εNd(t)-(87Sr/86Sr)i(底图据Wang et al., 2013）图解

    Figure 7. 

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    图 8  冷水坑花岗斑岩锆石原位εHf(t)-δ18O关系图解

    Figure 8. 

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    图 9  冷水坑花岗斑岩构造环境判别图解

    Figure 9. 

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    表 1  冷水坑矿床花岗斑岩锆石SHRIMP U-Pb年龄分析结果

    Table 1.  Results of zircon U-Pb SHRIMP dating of granite porphyry in the Lengshuikeng Pb-Zn deposit

    下载: 导出CSV

    表 2  冷水坑铅锌矿床花岗斑岩主量（%）、稀土及微量元素(10-6)分析结果

    Table 2.  Major, rare earth and trace element compositions of granite porphyry in the Lengshuikeng Pb-Zn deposit

    下载: 导出CSV

    表 3  冷水坑铅锌矿床花岗斑岩Sr-Nd同位素分析结果

    Table 3.  Sr-Nd isotope compositions of granite porphyry in the Lengshuikeng Pb-Zn deposit

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    表 4  冷水坑铅锌矿床花岗斑岩锆石原位Hf-O同位素组成

    Table 4.  Zircon in situ Hf-O isotopic composition of granite porphyry in the Lengshuikeng Pb-Zn deposit

    下载: 导出CSV
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收稿日期:  2019-04-18
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