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Petrology and ion microprobe U-Pb chronology applied to a metabasic intrusion in southern Sweden: A study on zircon formation during metamorphism and deformation

机译:岩石学和离子微探针U-Pb年代学在瑞典南部的一次基底侵入中的应用:变质和变形过程中锆石形成的研究

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摘要

The Aker metabasite occupies a key position in a major tectonic lineament in southernmost Sweden, the Protogine Zone, which coincides closely with the eastern boundary of the late Mesoproterozoic Sveconorwegian orogen of southwest Scandinavia. Metamorphic reactions, associated with the transformation from isotropic gabbro to foliated garnet amphibolite, were identified from disequilibrium textures of which some involved release of zirconium (Zr) and growth of metamorphic zircon. Ion microprobe dating of igneous zircon gave 1562 +- 6 Ma, whereas metamorphic zircons yielded ages of 1437+-21, 1217+-75, and 1006+-68 Ma.
机译:在瑞典最南端的一个主要构造地带的原生动物区中,Aker变质岩占据了关键位置,该区与斯堪的纳维亚半岛西南部中元古代的Sveconorwegian造山带的东部边界非常吻合。从各向同性辉长岩转变为叶状石榴石两闪石的变质反应是从不平衡结构中鉴定出来的,其中一些涉及锆(Zr)的释放和变质锆石的生长。火成锆石的离子微探针定年为1562±6 Ma,而变质锆石的年龄为1437 + -21、1217 + -75和1006 + -68 Ma。

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