首页> 外文期刊>Lithos: An International Journal of Mineralogy, Petrology, and Geochemistry >Multi-system geochronology of North Dabie eclogite: Ineffective garnet `shielding' on rutile inclusions under multi-thermal conditions
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Multi-system geochronology of North Dabie eclogite: Ineffective garnet `shielding' on rutile inclusions under multi-thermal conditions

机译:北大·蒙莱峰的多系统地理学论:多热条件下金红石包裹物中的无效石榴石“屏蔽”

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It has been shown that certain host minerals can robustly shield mineral inclusions and prevent loss of petrochronological information during subsequent thermal events. Ruble indusions in garnet may crystallize under a wide range of metamorphic conditions and thus ruble is expected to be a useful geochronometer for constraining different stages of a metamorphic P-T path. Hence, it is important to ascertain whether rutile inclusions shielded by garnet retain the original crystallization age information despite later retrograde cooling or subsequent new thermal events. In this study, we test the "shielding effect" of garnet on rutile inclusions from the Baizhangya edogite in the North Dabie Zone (China), which underwent a multi-stage thermal evolution. Secondary ion mass spectrometry (SIMS) U-Pb dating of inherited zircon core domains constrains a Neoproterozoic formation age (similar to 770 Ma) of the eclogite protolith. SIMS U-Pb dating of metamorphic zircon and complementary thermal-ionization mass spectrometry (TIMS) Sm-Nd isochron dating of garnet revealed Triassic eclogitefacies metamorphic ages (245-210 Ma). An Early Cretaceous SIMS U-Pb age of ca. 130 Ma. yielded by matrix rutile grains and rutile inclusions, suggests significant isotopic alteration since crystallization. This indicates that shielding was ineffective, since the U-Pb ages derived from the rutile inclusions, although hermetically armored by garnet, were influenced by a subsequent Early Cretaceous tectono-thermal event. Further transmission electron microscope (TEM) analysis revealed the presence of hematite microlites along the garnet-rutile boundaries, which may have acted as a potential reservoir to store the expelled radiogenic Pb from Mile. This study suggests that newly formed minerals located along mineral boundaries seem to be crucial for understanding the shielding effect. (C) 2020 Elsevier B.V. All rights reserved.
机译:已经表明,某些宿主矿物质可以在随后的热事件期间防止矿物质夹杂物和防止岩石学信息的损失。石榴石中的卢布凝结可以在各种变质条件下结晶,因此预计鲁布将是用于约束变质P-T路径的不同阶段的有用的地球数。因此,尽管以后逆行冷却或随后的新热事件,但是,重要的是要确定由石榴石屏蔽的金红石夹杂物是否保留原始结晶年龄信息。在这项研究中,我们在北大迪亚(中国)中的Baizhangya Feoogite中的金红石内含物上的“屏蔽效应”测试了北大大区(中国)的金红石夹杂物。继承锆石核心区段的二次离子质谱(SIMS)U-PB约会约束Eclogite促果的新中间超古代形成年龄(类似于770mA)。 SIMS U-PB变形锆石和互补热电电离质谱(TIMS)SM-ND同种编织Garnet的SM-ND同胞介绍,揭示了三叠系欧洲斑缺陷变质年龄(245-210 mA)。早期的白垩纪SIMS U-PB年龄。 130 mA。由基质金红石颗粒和金红石夹杂物产生,表明自结晶以来显着的同位素改变。这表明屏蔽是无效的,因为虽然由石榴石沉默的熔丝夹杂物衍生的U-Pb年龄源于后续早期的白垩纪的Tectono-热事件,但是源于金红石夹杂物。进一步的透射电子显微镜(TEM)分析显示沿石榴石边界的赤铁矿微岩的存在,其可以充当潜在的储层,以将排出的辐射PB从英里储存。本研究表明,位于矿物边界的新形成矿物似乎对理解屏蔽效果至关重要。 (c)2020 Elsevier B.V.保留所有权利。

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