Global distribution of the HIMU end member: Formation through Archean plume-lid tectonics
Oceanic basalts reflect the heterogeneities in the earth's mantle, which can be explained by five mantle end members. The HIMU end member, characterized by high time-integrated μ (238U/204Pb), is defined by the composition of lavas from the ocean islands of St. Helena, South Atlantic Ocean and...
Published in: | Earth-Science Reviews |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier
2018
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Subjects: | |
Online Access: | https://oceanrep.geomar.de/id/eprint/42981/ https://oceanrep.geomar.de/id/eprint/42981/1/Homrighausen.pdf https://oceanrep.geomar.de/id/eprint/42981/7/Homrighausen.pdf https://doi.org/10.1016/j.earscirev.2018.04.009 |