秦岭拉鸡庙镁铁质岩体锆石LA-ICP-MS年代学研究

刘军锋, 孙勇, 孙卫东. 秦岭拉鸡庙镁铁质岩体锆石LA-ICP-MS年代学研究[J]. 岩石学报, 2009, 25(2): 320-330.
引用本文: 刘军锋, 孙勇, 孙卫东. 秦岭拉鸡庙镁铁质岩体锆石LA-ICP-MS年代学研究[J]. 岩石学报, 2009, 25(2): 320-330.
LIU JunFeng, SUN Yong, SUN WeiDong. LA-ICP-MS zircon dating from the Lajimiao mafic complex in the Qinling orogenic belt[J]. Acta Petrologica Sinica, 2009, 25(2): 320-330.
Citation: LIU JunFeng, SUN Yong, SUN WeiDong. LA-ICP-MS zircon dating from the Lajimiao mafic complex in the Qinling orogenic belt[J]. Acta Petrologica Sinica, 2009, 25(2): 320-330.

秦岭拉鸡庙镁铁质岩体锆石LA-ICP-MS年代学研究

  • 基金项目:

    国家973计划项目"华北大陆边缘造山过程与成矿"(2006CB403500), 杰出青年基金(40525010) 和国家自然基金(40773044)

LA-ICP-MS zircon dating from the Lajimiao mafic complex in the Qinling orogenic belt

  • 秦岭拉鸡庙镁铁质岩体位于北秦岭南缘,主要由辉长岩(80%)、苏长辉长岩(15%)和少量闪长岩等侵入杂岩组成。对采自该岩体闪长岩的锆石进行阴极发光图像、微区原位LA-ICP-MS微量元素分析和U-Pb定年。CL图像显示这些锆石可以分为两类,一类锆石呈长柱状,具有明显的岩浆生长环带;另一类则呈浑圆状,阴极发光图像复杂,部分颗粒岩浆生长环带较模糊,个别样品外围存在一窄的亮色环边,推测为后期地质事件影响的结果。对26颗锆石核部和生长边进行28次U-Pb同位素分析,获得两组206Pb/238U年龄,分别为973±60Ma和422±7Ma。分析结果显示,所有样品具有高的Th, U, REE含量,明显富集HREE,其Th/U比值普遍高于0.6,表明这些锆石应属于岩浆成因。其中,422±7Ma应该代表拉鸡庙镁铁质岩体的成岩时代,这可能与古生代扬子陆块或者是具有扬子板块属性的微陆块和华北陆块的碰撞有关,该碰撞导致了秦岭洋的闭合;而973±60Ma应为捕获锆石年龄,代表北秦岭早期与Rodinia超大陆拼合有关的岩浆事件。考虑到没有检测到典型的华北克拉通的年龄,推测元古代北秦岭更接近华南板块。
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出版历程
收稿日期:  2008-09-23
修回日期:  2008-12-02
刊出日期:  2009-02-28

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