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首页> 外文期刊>International Journal of Earth Sciences >Discovery of an albite gneiss from the He de Groix (Armorican Massif, France): geochemistry and LA-ICP-MS U-Pb geochronology of its Ordovician protolith
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Discovery of an albite gneiss from the He de Groix (Armorican Massif, France): geochemistry and LA-ICP-MS U-Pb geochronology of its Ordovician protolith

机译:从He de Groix(法国Armorican Massif)发现的钠长石片麻岩:奥陶纪原生岩的地球化学和LA-ICP-MS U-Pb地球年代学

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摘要

For the first time, an albite orthogneiss has been recognised and dated within the HP-LT blueschist facies metabasites and metapelites of the He de Groix. It is charac-terised by a peraluminous composition, high LILE, Th and U contents, MORB-like HREE abundances and moderate Nb and Y values. A U-Pb age of 480.8 ± 4.8 Ma was obtained by LA-ICP-MS dating of zircon and titanite. It is interpreted as the age of the magmatic emplacement during the Early Ordovician. Morphologically different zircon grains yield late Neoproterozoic ages of 546.6-647.4 Ma. Zircon and titanite U-Pb ages indicate that the felsic magmatism from the lie de Groix is contemporaneous with the acid, pre-oro-genic magmatism widely recognised in the internal zones of the Variscan belt, related to the Cambro-Ordovician conti-nental rifting. The magmatic protolith probably inherited a specific chemical composition from a combination of oro-genic, back-arc and anorogenic signatures because of partial melting of the Cadomian basement during magma emplace-ment. Besides, the late Devonian U-Pb age of 366 ± 33 Ma obtained for titanite from a blueschist facies metapelite cor-responds to the age of the HP-LT peak metamorphism.
机译:第一次,在赫德格罗瓦河的HP-LT蓝胶岩相陆生变质岩和变质岩中,钠长石正长片岩被认识并确定了日期。它具有高铝质成分,高LILE,Th和U含量,MORB样HREE丰度和适中的Nb和Y值的特点。通过锆石和钛矿的LA-ICP-MS测年获得了480.8±4.8 Ma的U-Pb年龄。它被解释为奥陶纪早期的岩浆侵位时代。形态不同的锆石晶粒产生的新元古代晚期年龄为546.6-647.4 Ma。锆石和钛铁矿的U-Pb年龄表明,Lie de Groix的长英质岩浆作用与瓦里斯卡纳带内部地区广泛认可的酸性,早成因岩浆作用同时发生,与坎布罗-奥陶纪大陆陆裂有关。岩浆原生岩可能是由于成岩作用期间Cadomian基底的部分融化而从造山带,后弧和厌食信号的组合中继承了特定的化学成分。此外,从蓝片岩相变质变质岩中的钛矿获得的泥盆纪晚期U-Pb年龄为366±33 Ma,对应于HP-LT峰变质的年龄。

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