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现代地质 ›› 2018, Vol. 32 ›› Issue (04): 667-679.DOI: 10.19657/j.geoscience.1000-8527.2018.04.04

• 岩石学 • 上一篇    下一篇

中祁连西段石板墩堆晶岩的地球化学特征及构造意义

马蓁(), 刘铮, 刘懿馨, 王金荣()   

  1. 兰州大学 地质科学与矿产资源学院 甘肃省西部矿产资源重点实验室,甘肃 兰州 730000
  • 收稿日期:2017-08-07 修回日期:2017-12-23 出版日期:2018-08-10 发布日期:2018-09-19
  • 通讯作者: 王金荣
  • 作者简介:王金荣,男,教授,博士生导师,1957年出生,矿物学、岩石学、矿床学专业,主要从事岩石学和大地构造研究工作。Email: jrwang@lzu.edu.cn
    马 蓁,女,博士研究生,1988年出生,矿物学、岩石学、矿床学专业,主要从事岩石学和大地构造研究工作。Email:mazhen34@163.com
  • 基金资助:
    甘肃省科技重大专项计划项目“甘肃省肃北石板墩大型磁铁矿地质找矿方法技术研究”(1002FKDA04);中央高校基本科研业务费专项资金(lzujbky-2016 -197)

Geochemical Characteristics and Tectonic Significance of Shibandun Mafic-ultramafic Cumulates in Western Part of the Central Qilian

MA Zhen(), LIU Zheng, LIU Yixin, WANG Jinrong()   

  1. School of Earth Sciences,Lanzhou University,Key Laboratory of Mineral Resources in Western China,Lanzhou, Gansu 730000,China
  • Received:2017-08-07 Revised:2017-12-23 Online:2018-08-10 Published:2018-09-19
  • Contact: WANG Jinrong

摘要:

石板墩堆晶岩位于中祁连地块西段党河断裂带北侧,主要由橄榄岩、蛇纹石化橄辉岩和辉长岩组成,具有多旋回、多韵律层的产出特征。辉长岩LA-ICP-MS锆石U-Pb年龄为(486.5 ± 3.3) Ma。岩石地球化学结果显示,蛇纹石化橄辉岩和辉长岩配分型式十分相似,具有富集大离子亲石元素、亏损高场强元素、LREE相对富集、HREE平坦型分布以及正Eu异常(Eu/Eu*=0.97~3.04)的特点。研究结果表明,蛇纹石化橄辉岩、辉长岩为同源岩浆作用的产物,源区为被俯冲流体交代过的软流圈地幔,形成于火山弧环境,是在岩浆作用过程中不断发生堆晶作用,并在堆晶之后再次泵入混合大量新的玄武岩浆反复进行所形成。结合区域大地构造背景,认为中祁连西段是早古生代早期在残留的微陆块基础上形成的一个火山弧增生杂岩地体。

关键词: 堆晶岩, 石板墩地区, 中祁连西段, 早古生代, 火山弧增生杂岩地体

Abstract:

The Shibandun mafic-ultramafic cumulates are widely distributed in the western part of the Central Qilian, north of the Danghenanshan fault zone. The mafic-ultramafic cumulates comprise multiple sequences of (from bottom to top) peridotite, olivine pyroxenite, gabbro, magnetite and diorite. LA-ICP-MS zircon U-Pb dating of the gabbro yielded a mean 206Pb/238U age of (486.5±3.3) Ma. Geochemical analysis indicates that serpentinized olivine pyroxenite has similar multi-element patterns to the gabbros, and they both show large ion lithophile element (LILE) enrichments and high field strength element (HFSE) depletions. They are also relatively enriched in LREE, and with flat HREE patterns and positive Eu anomalies (0.97-3.64). The study shows that the Shibandun mafic-ultramafic cumulates were likely co-magmatic, and the magma was likely derived from the subduction fluid-metasomatized asthenospheric mantle.The magmatic evolution process may have involved repeated cycles of magma fractionation, cumulate formation and basaltic magma replenishment.The Shibandunmafic-ultramafic cumulates were likely formed in volcanic arc setting.Integrated with the regional tectonic background, we propose that the western part of the Central Qilian microcontinent was likely a volcanic arc accretionary complex that was formed on the residual microcontinental margin.

Key words: cumulate, Shibandun, western part of the Central Qilian, Early Paleozoic, volcanic arc accretionary complex

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