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现代地质 ›› 2018, Vol. 32 ›› Issue (06): 1242-1253.DOI: 10.19657/j.geoscience.1000-8527.2018.06.12

• 岩石学 • 上一篇    下一篇

华北克拉通东南缘蚌埠隆起带荆山—涂山岩体地质地球化学特征再认识

康丛轩1,2(), 杨献忠1, 蔡逸涛1, 宗雯3, 黄先觉4, 孔广林4, 李朝维4   

  1. 1.中国地质调查局 南京地质调查中心,江苏 南京 210016
    2.河海大学 地球科学与工程学院,江苏 南京 211100
    3.江苏省地质调查研究院,江苏 南京 210018
    4.安徽省地质矿产勘查局312地质队,安徽 蚌埠 233040
  • 收稿日期:2017-10-11 修回日期:2018-05-23 出版日期:2018-12-10 发布日期:2018-12-20
  • 作者简介:康丛轩,男,博士研究生,助理研究员,1985年出生,矿物学、岩石学、矿床学专业,主要从事矿物岩石及工程地质研究。Email:kangcongxuan@sina.com
  • 基金资助:
    安徽省公益性地质调查基金项目(2014-K-5)

Review of Geochemical Characteristics of Jingshan-Tushan Granites in Bengbu Uplift, Southeast Margin of North China Craton

KANG Congxuan1,2(), YANG Xianzhong1, CAI Yitao1, ZONG Wen3, HUANG Xianjue4, KONG Guanglin4, LI Chaowei4   

  1. 1. Nanjing Center of Geological Survey, China Geology Survey, Nanjing, Jiangsu 210016, China
    2. School of Earth Sciences and Engineering, Hohai University, Nanjing, Jiangsu 211100, China
    3. Geological Survey of Jiangsu Province, Nanjing, Jiangsu 210018, China
    4. Geological Team 312,Bureau of Geology and Mineral Resources Exploration in Anhui Province, Bengbu, Anhui 233040, China
  • Received:2017-10-11 Revised:2018-05-23 Online:2018-12-10 Published:2018-12-20

摘要:

对位于华北克拉通东南缘蚌埠隆起带的荆山—涂山岩体进行了野外观察、年代学和地球化学研究,测得弱片麻状二长花岗岩体中U-Pb年龄为(160.4±1.3)~(162.8±1.8) Ma,为晚侏罗世岩浆活动的产物;岩石地球化学测试结果显示,岩体总体富硅、富碱,具有高钾钙碱、准铝—过铝质特征,LREE相对富集,具明显的正Eu异常,Ce异常不明显或无异常,K、P和Ti有较明显的亏损,Rb、Ba、U、La、Sr、Zr和Sm元素相对富集。成因类型判别图显示其具备I型花岗岩特征;锆石Lu-Hf同位素及全岩Sm-Nd同位素组成暗示其物质起源主要为新太古代陆壳,且岩浆源区主要为华北克拉通下地壳物质;构造环境判别图中,投影点落于火山弧花岗岩区域,暗示岩体形成于扬子克拉通沿郯庐断裂带俯冲于华北克拉通之下的构造背景,与华北克拉通晚侏罗世期间的动力学背景相一致。

关键词: 华北克拉通, 蚌埠隆起带, 荆山—涂山岩体, 地球化学特征

Abstract:

In this study, we carried out field observation, geochronological and geochemical analyses on the Jingshan-Tushan granites in the Bengbu uplift, southern margin of the North China craton. Zircon U-Pb dating of the weakly-gneissic monzogranite yielded (160.4±1.3) Ma to (162.8±1.8) Ma, suggesting Late Jurassic magmatism. Lithogeochemical data show that the Jingshan-Tushan granites are overall Si- and alkali-rich, high-K calc-alkaline, metaluminous-peraluminous, relatively LREE-enriched, with strong positive Eu anomalies and subtle Ce anomalies. The granites are also depleted in K, P and Ti, and relatively enriched in Rb, Ba, U, La, Sr, Zr and Sm. Data points of the granites fall into the I-type field in the petrogenetic discrimination diagram, and zircon Lu-Hf and whole-rock Sm-Nd compositions suggest that the magma source may have been mainly derived from the Neoarchean continental crust. In tectonic discrimination diagrams, the data points fall mainly in the volcanic arc granite field. It is suggested that the granites were formed in a post-collision extensional setting, consistent with the geodynamic background of the Late Jurassic North China craton.

Key words: North China Craton, Bengbu uplift, Jingshan-Tushan granite, lithogeochemical characteristic

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