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川陕交界地区刘家坪花岗岩年代学、地球化学特征及构造意义

胡安新, 孙丰月, 王英德, 刘金龙, 张亮, 李良

胡安新, 孙丰月, 王英德, 等. 川陕交界地区刘家坪花岗岩年代学、地球化学特征及构造意义[J]. 西北地质, 2014, 47(2): 30-40.
引用本文: 胡安新, 孙丰月, 王英德, 等. 川陕交界地区刘家坪花岗岩年代学、地球化学特征及构造意义[J]. 西北地质, 2014, 47(2): 30-40.
HU An-xin, SUN Feng-yue, WANG Ying-de, et al. Geochronological and Geochemical Study on Liujiaping Granite in the Border Area between Sichuan and Shaanxi Province and Its Tectonic Significance[J]. Northwestern Geology, 2014, 47(2): 30-40.
Citation: HU An-xin, SUN Feng-yue, WANG Ying-de, et al. Geochronological and Geochemical Study on Liujiaping Granite in the Border Area between Sichuan and Shaanxi Province and Its Tectonic Significance[J]. Northwestern Geology, 2014, 47(2): 30-40.

川陕交界地区刘家坪花岗岩年代学、地球化学特征及构造意义

基金项目: 

陕西盛安矿业开发有限公司陕西省宁强县鸡头山—小燕子沟金矿床矿化富集规律及成矿预测研究(2013220101000019)

详细信息
    作者简介:

    胡安新(1988- ),男,硕士研究生,矿产普查与勘探专业。E-mail:hax1988@qq.com

  • 中图分类号: P595

Geochronological and Geochemical Study on Liujiaping Granite in the Border Area between Sichuan and Shaanxi Province and Its Tectonic Significance

  • 摘要: 对川陕交界地区刘家坪花岗岩岩体进行了系统的锆石U-Pb年代学和地球化学研究,重点讨论了岩体的成因及其构造意义。测试结果显示,刘家坪花岗岩加权平均年龄值为825.9±7.8 Ma,属新元古代中期;岩石低K富Na,显示硅过饱和,w(SiO2)%平均为75.32,并伴有过Al质特征;稀土元素丰度较低,∑REE为(182.13~243.76)×10-6,平均为197.29×10-6,显示LREE富集、HREE相对亏损的特征,稀土元素球粒陨石配分模式图表现为右倾“海鸥”型,并且具有明显的Eu负异常(δEu平均为0.57);微量元素中Nb/Ta、Rb/Sr的结果及Mg#值综合显示岩浆来源主要为下地壳物质的部分熔融。岩石具有A型花岗岩特征,形成于碰撞期后的伸展构造背景,据此推测碧口地块与扬子地块在825 Ma之前曾发生碰撞造山作用。两者的拼合模式为从北东到南西的剪刀式拼合。
    Abstract: The Liujiaping granite intrusion is located in Sichuan-Shaanxi border area. The study of the zircon U-Pb geochronology and the geochemistry of the granite aim at discussing its formation and tectonic significance. The results show that the crystallization age of the granite is 825.9±7.8 Ma, which belongs to the mid-Neoproterozoic. The geochemistry analysis shows that the intrusion is low in potassium and rich in sodium and silica (with the average SiO2 being 75.32%), with peraluminous characteristics. The abundance of the ∑REE varies in the range of (182.13-243.76)×10-6, with 197.29×10-6 on average, which shows an enrichment of the LREE and a depletion of the HREE. Chondrite-normalized REE patterns are of the right sea-gull oblique type with the δEu being 0.57, showing a significant negative Eu anomaly. The results of the Nb/Ta, Rb/Sr and Mg# show that the magmatic rocks of this region originated from the partial melting of the lower crust. With the characteristics of A type granites, the rock formed in the post-collision extensional tectonic setting, which indicates a collision had occurred between the Eastern Bikou terrane and the Yangtze block before 825Ma. The jointing mode of the two blocks is scissors joint from northeast to southwest.
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出版历程
  • 收稿日期:  2014-02-23
  • 修回日期:  2014-04-07
  • 网络出版日期:  2022-07-28
  • 发布日期:  2014-06-04

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