河北承德大庙地区元古代的晚期辉长—苏长岩的岩石特征及其成因

路智, 刘永顺, 聂保锋, 王仁民. 2022. 河北承德大庙地区元古代的晚期辉长—苏长岩的岩石特征及其成因. 地质科学, 57(1): 243-261. doi: 10.12017/dzkx.2022.015
引用本文: 路智, 刘永顺, 聂保锋, 王仁民. 2022. 河北承德大庙地区元古代的晚期辉长—苏长岩的岩石特征及其成因. 地质科学, 57(1): 243-261. doi: 10.12017/dzkx.2022.015
Lu Zhi, Liu Yongshun, Nie Baofeng, Wang Renmin. 2022. Petrological characteristics and genesis of Late Proterozoic gabbro-norite in Damiao area, Chengde, Hebei Province. Chinese Journal of Geology, 57(1): 243-261. doi: 10.12017/dzkx.2022.015
Citation: Lu Zhi, Liu Yongshun, Nie Baofeng, Wang Renmin. 2022. Petrological characteristics and genesis of Late Proterozoic gabbro-norite in Damiao area, Chengde, Hebei Province. Chinese Journal of Geology, 57(1): 243-261. doi: 10.12017/dzkx.2022.015

河北承德大庙地区元古代的晚期辉长—苏长岩的岩石特征及其成因

  • 基金项目:

    国家自然科学基金项目(编号:41641017)资助。

详细信息
    作者简介:

    路智,男,1986年生,硕士,自然地理学专业。E-mail:854227111@qq.com

    通讯作者: 刘永顺,男,1966年生,博士,副教授,岩石学专业。本文通讯作者。E-mail:cnu901@126.com
  • 中图分类号: P584;P588.12

Petrological characteristics and genesis of Late Proterozoic gabbro-norite in Damiao area, Chengde, Hebei Province

More Information
  • 河北承德的大庙斜长岩杂岩体是我国著名的岩体型斜长岩杂岩体,其苏长岩可分为两种类型,即早期苏长岩和晚期辉长—苏长岩。早期苏长岩已发生钠长绿帘角闪岩相变质;晚期辉长—苏长岩变质程度较弱,含有斜长石、斜方辉石和单斜辉石巨晶,主要呈岩墙、岩脉或小岩体侵入于斜长岩杂岩体中,与铁磷矿紧密相关。研究表明:晚期辉长—苏长岩主要由中性斜长石、反条纹长石、单斜辉石、斜方辉石、黑云母、磷灰石、钛磁铁矿和磁铁矿等组成,依矿物含量、成分和结构的差异可分为淡色辉长岩、单斜辉石苏长岩、斜方辉石辉长岩以及含铁磷矿对应岩石。其Ba、Sr和轻稀土富集、Eu弱负异常或无异常特征,表明晚期辉长—苏长岩岩浆不是形成斜长岩的基性岩浆,而是经斜长石分离结晶后的残余岩浆。Sr-Nd-Pb同位素地球化学特征显示晚期辉长—苏长岩可能源自EMI富集的岩石圈地幔,与岩体型斜长岩不存在同源岩浆分离结晶演化的关系。大庙地区晚期辉长—苏长岩的岩浆来源、演化和构造控制的特征对深化研究岩体型斜长岩杂岩体的成因有重要意义。
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收稿日期:  2020-05-22
修回日期:  2021-09-07

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