医巫闾山地区早白垩世同伸展花岗岩就位机制

李刚, 刘正宏, 崔维龙, 白相东. 医巫闾山地区早白垩世同伸展花岗岩就位机制[J]. 岩石学报, 2016, 32(9): 2677-2689.
引用本文: 李刚, 刘正宏, 崔维龙, 白相东. 医巫闾山地区早白垩世同伸展花岗岩就位机制[J]. 岩石学报, 2016, 32(9): 2677-2689.
LI Gang, LIU ZhengHong, CUI WeiLong, BAI XiangDong. Emplacement of Early Cretaceous syn-extension granitic in Yiwulüshan area, North China[J]. Acta Petrologica Sinica, 2016, 32(9): 2677-2689.
Citation: LI Gang, LIU ZhengHong, CUI WeiLong, BAI XiangDong. Emplacement of Early Cretaceous syn-extension granitic in Yiwulüshan area, North China[J]. Acta Petrologica Sinica, 2016, 32(9): 2677-2689.

医巫闾山地区早白垩世同伸展花岗岩就位机制

  • 基金项目:

    本文受国家自然科学基金项目(41272223、41402169、41340024)资助.

Emplacement of Early Cretaceous syn-extension granitic in Yiwulüshan area, North China

  • 石山岩体形成的时间约为124Ma,是医巫闾山地区早白垩世NWW向伸展变形的同构造花岗岩体。花岗岩的主量、微量元素含量表现出埃达克质岩浆的特点,SiO2、Al2O3及碱性组分含量较高,而Fe2O3T和MgO含量较低,岩浆锆石εHf(t)值=-26.7~-20.3、tDM2=2.0~2.3Ga,表明岩浆来源于华北陆块加厚下地壳的部分熔融。通过对围岩变形组构与岩体中岩浆组构的分析,可将石山岩体的就位过程划分为三个阶段。在岩浆底劈、膨胀作用和围岩伸展滑移的共同影响下,石山岩体最终形成了主体呈近圆形、西部发育两个岩墙的形态。岩浆就位过程与围岩变形组构的相互关系,表明中、浅部地壳的伸展变形可以控制岩浆的就位过程和最终形态,但与下地壳部分熔融的关系不大,岩石圈减薄及区域伸展应力场是下地壳发生部分熔融的诱因。
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出版历程
收稿日期:  2016-03-21
修回日期:  2016-06-30
刊出日期:  2016-09-30

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