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Acasta片麻杂岩多期次热事件:来自锆石、榍石和磷灰石的原位微区年代学证据 被引量:1

Multiple thermal events recorded in the Acasta Gneiss Complex:Evidence from in-situ dating of zircon,titanite,and apatite
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摘要 本文使用激光剥蚀电感耦合等离子体质谱(LA-ICPMS)和二次离子质谱(SIMS)对Acasta片麻杂岩样品碎片(大小约1cm2)中的锆石、磷灰石和榍石进行了原位微区定年,以制约Acasta片麻杂岩的热演化历史.这些样品碎片中的锆石显示多期年龄,反映了继承锆石的存在或者锆石结晶后的再生长过程.结合前人研究,本文锆石数据揭示, Acasta片麻杂岩经历的多期岩浆事件发生时间分别为:>3.96、约3.72和约3.57Ga.样品AY199中榍石的PbPb等时线年龄为(2911±22)Ma(95%置信水平, MSWD=1.5),与Acasta片麻杂岩记录的太古宙最后一次岩浆事件年龄一致.样品AC478和AY066中榍石U-Pb年龄分别为(1932±270)Ma(95%置信水平, MSWD=2.3)和(1813±45)Ma(95%置信水平, MSWD=2.3).样品P090803-C中磷灰石的Pb-Pb等时线年龄为(1833±26)Ma(95%置信水平,MSWD=1.4).样品AC478、AY199和AY066中磷灰石U-Pb年龄分别为(1850±20)Ma(95%置信水平, MSWD=1.3)、(1827±100)Ma(95%置信水平, MSWD=6.3)和(1807±58)Ma(95%置信水平, MSWD=3.9).样品AC478和AY066中的榍石U-Pb年龄以及本文所有样品中的磷灰石Pb-Pb或U-Pb年龄相同,均为约1.9~1.8Ga,指示Wopmay造山作用导致的矿物U-Pb体系重置,证明了Wopmay造山作用的峰期温度超过了磷灰石的U-Pb体系封闭温度,并接近或者超过榍石的U-Pb体系封闭温度.
作者 梅清风 杨进辉 孙金凤 李秋立 吴石头 凌潇潇 彭澎 王浩 Mei Q;Yang J;Sun J;Li Q;Wu S;Ling X;Peng P;Wang H
出处 《中国科学:地球科学》 CSCD 北大核心 2024年第3期693-707,共15页 Scientia Sinica(Terrae)
基金 国家自然科学基金项目(批准号:42103011、42073034、42288201) 中国科学院战略性先导科技专项(B类)项目(编号:XDB41000000)资助。
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