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首页> 外文期刊>Contributions to Mineralogy and Petrology >Behaviour of zircon in high-grade metamorphic rocks: evidence from Hf isotopes, trace elements and textural studies
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Behaviour of zircon in high-grade metamorphic rocks: evidence from Hf isotopes, trace elements and textural studies

机译:锆石在高级变质岩中的行为::同位素,微量元素和组织学研究的证据

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摘要

Hf isotopic data of minerals in a mafic pyroxene granulite from the southern Bohemian Massif, together with their major and trace element composition and pet-rological observations were used to decipher the metamorphic history and behaviour of zircon in the granulite. The Hf isotopic composition in the minerals was used to estimate whether the decompression reaction, namely the consumption of garnet and rutile, could have provided Zr for the formation of newly grown metamorphic zircon. The age of the decompression reaction indicated by the evolution of Hf isotopes in garnet and orthopyroxene is between 333 and 331 Ma, i.e. ca. 7 Ma younger than the available U-Pb zircon ages from the Moldanubian granulites and than the newly obtained 343 + - 2 Ma laser ablation ICP-MS U-Pb age of zircons. The combination of bulk and in-situ Hf isotopic data, major and trace element composition and petrological modeling of P-T evolution revealed that the formation of zircons can not be related to the decompression phase of the evolution of the mafic granulites.
机译:来自波希米亚地块南部的镁铁质辉石质花岗石中矿物的Hf同位素数据,以及其主要和微量元素组成以及岩石学观测资料,用于解释该花岗石中锆石的变质历史和行为。矿物中的Hf同位素组成用于评估减压反应(即石榴石和金红石的消耗)是否可以为新近形成的变质锆石的形成提供Zr。石榴石和邻苯二酚中H同位素的演变表明减压反应的年龄在333至331 Ma之间,即大约比摩尔达努比亚花岗石中可用的U-Pb锆石年龄小7 Ma,并且比新获得的343 +-2 Ma激光烧蚀ICP-MS锆石年龄小7 Ma。大量和原位Hf同位素数据,主要和微量元素组成以及P-T演化的岩石学模型的结合表明,锆石的形成与镁铁质粒岩演化的减压阶段无关。

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