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DOI10.1016/j.epsl.2020.116323
HIMU geochemical signature originating from the transition zone
Huang S.; Tschauner O.; Yang S.; Humayun M.; Liu W.; Gilbert Corder S.N.; Bechtel H.A.; Tischler J.
发表日期2020
ISSN0012821X
卷号542
英文摘要Plume volcanism may sample mantle sources deeper than mid-ocean ridge and arc volcanism. Ocean island basalts (OIBs) are commonly related to plume volcanism, and their diverse isotopic and elemental compositions can be described using a limited number of mantle endmembers. However, the origins and depths of these mantle endmembers are highly debated. Here we show that the HIMU (high μ, μ=238U/204Pb) endmember may reside in the transition zone. Specifically, we report the geochemical signature of a high-pressure multiphase diamond inclusion, entrapped at 420–440 km depth and 1450 ± 50 K, which matches exactly the geochemical patterns of the HIMU-rich OIBs. Since the HIMU component is variably sampled by almost all OIBs, our finding implies that the transition zone causes a major overprint of the geochemical features of mantle plumes. Some mantle plumes, like those feeding Bermuda, St Helena, Tubuai and Mangaia, appear to be dominated by this source. Furthermore, our finding highlights the importance of the transition zone in highly incompatible element budget of the mantle. © 2020 Elsevier B.V.
关键词diamond inclusionhigh-pressure mineralsHIMUmantle plumestrace elementstransition zone
英文关键词Budget control; Diamond deposits; Thermal plumes; Diamond inclusions; Elemental compositions; Geochemical features; Geochemical patterns; Geochemical signatures; Incompatible element; Mantle endmembers; Ocean island basalts; Geochemistry; igneous geochemistry; igneous intrusion; isotopic composition; mantle plume; transition zone; volcanism; Saint Helena
语种英语
来源期刊Earth and Planetary Science Letters
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/202661
作者单位Department of Geoscience, University of Nevada Las Vegas, Las Vegas, NV 89154, United States; National High Magnetic Field Laboratory, Department of Earth, Ocean & Atmospheric Science, Florida State University, Tallahassee, FL 32310, United States; Advanced Photon Source, Argonne National Laboratory, Lemont, IL 60439, United States; Advanced Light Source, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, United States
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Huang S.,Tschauner O.,Yang S.,et al. HIMU geochemical signature originating from the transition zone[J],2020,542.
APA Huang S..,Tschauner O..,Yang S..,Humayun M..,Liu W..,...&Tischler J..(2020).HIMU geochemical signature originating from the transition zone.Earth and Planetary Science Letters,542.
MLA Huang S.,et al."HIMU geochemical signature originating from the transition zone".Earth and Planetary Science Letters 542(2020).
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