中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Multi-system geochronology of North Dabie eclogite: Ineffective garnet `shielding' on rutile inclusions under multi-thermal conditions

文献类型:期刊论文

作者Zhou, Tian2,4,5; Li, Qiuli2,4,5; Klemd, Reiner1; Shi, Yonghong3; Tang, Xu5; Li, Chaofeng4,5; Liu, Yu4,5
刊名LITHOS
出版日期2020-09-01
卷号368页码:10
ISSN号0024-4937
关键词Shielding effect Ruble inclusions Secondary ion mass spectrometry U-Pb dating Transmission electron microscope
DOI10.1016/j.lithos.2020.105573
英文摘要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.
WOS关键词U-PB AGES ; EAST-CENTRAL CHINA ; ULTRAHIGH-PRESSURE METAMORPHISM ; TRACE-ELEMENT ; SM-ND ; MONAZITE INCLUSIONS ; CONTINENTAL-CRUST ; COOLING HISTORY ; EDOUGH MASSIF ; ZIRCON AGES
资助项目National Key Research and Development Program of China[2016YFE0203000] ; National Natural Science Foundation of China[41773044] ; National Natural Science Foundation of China[41673059] ; National Program for Support of Top-notch Young Professionals
WOS研究方向Geochemistry & Geophysics ; Mineralogy
语种英语
出版者ELSEVIER
WOS记录号WOS:000541261600003
资助机构National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals ; National Program for Support of Top-notch Young Professionals
源URL[http://ir.iggcas.ac.cn/handle/132A11/97154]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Li, Qiuli
作者单位1.Univ Erlangen Nurnberg, Schlossgarten 5a, D-91054 Erlangen, Germany
2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
3.Hefei Univ Technol, Sch Resources & Environm Engn, Hefei 230029, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
5.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Zhou, Tian,Li, Qiuli,Klemd, Reiner,et al. Multi-system geochronology of North Dabie eclogite: Ineffective garnet `shielding' on rutile inclusions under multi-thermal conditions[J]. LITHOS,2020,368:10.
APA Zhou, Tian.,Li, Qiuli.,Klemd, Reiner.,Shi, Yonghong.,Tang, Xu.,...&Liu, Yu.(2020).Multi-system geochronology of North Dabie eclogite: Ineffective garnet `shielding' on rutile inclusions under multi-thermal conditions.LITHOS,368,10.
MLA Zhou, Tian,et al."Multi-system geochronology of North Dabie eclogite: Ineffective garnet `shielding' on rutile inclusions under multi-thermal conditions".LITHOS 368(2020):10.

入库方式: OAI收割

来源:地质与地球物理研究所

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