Geochemical characteristics and origin of the HIMU reservoir: A possible mantle plume source in the lower mantle
Article first published online: 26 FEB 2011
Copyright 2011 by the American Geophysical Union.
Geochemistry, Geophysics, Geosystems
Volume 12, Issue 2, February 2011
How to Cite
2011), Geochemical characteristics and origin of the HIMU reservoir: A possible mantle plume source in the lower mantle, Geochem. Geophys. Geosyst., 12, Q0AC09, doi:10.1029/2010GC003252., et al. (
- Issue published online: 26 FEB 2011
- Article first published online: 26 FEB 2011
- Manuscript Accepted: 21 DEC 2010
- Manuscript Revised: 4 OCT 2010
- Manuscript Received: 10 JUN 2010
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|ggge1817-sup-0001-readme.txt||plain text document||2K||readme.txt|
|ggge1817-sup-0002-txts01.doc||Word document||86K||Text S1. Geological settings, sample preparation and analytical techniques, and major and trace element compositions of whole rocks and mineral separates.|
|ggge1817-sup-0003-ds01.xls||application/excel||42K||Data Set S1. Major and trace element compositions and mineral modes of the whole-rock samples with the information on sampling locations.|
|ggge1817-sup-0004-ds02.xls||application/excel||45K||Data Set S2. Average major element compositions of olivine and clinopyroxene.|
|ggge1817-sup-0005-ds03.xls||application/excel||31K||Data Set S3. Element compositions of clinopyroxene samples.|
|ggge1817-sup-0006-fs01.pdf||PDF document||52K||Figure S1. Trace element concentrations normalized to primitive upper mantle.|
|ggge1817-sup-0007-fs02.pdf||PDF document||39K||Figure S2. Plots of K2O versus P2O5 for the whole-rock samples.|
|ggge1817-sup-0008-fs03.pdf||PDF document||154K||Figure S3. Major element compositions of olivines.|
|ggge1817-sup-0009-fs04.pdf||PDF document||49K||Figure S4. Clinopyroxene/melt concentration ratios for REE.|
|ggge1817-sup-0010-fs05.pdf||PDF document||57K||Figure S5. Plots of Os concentrations and 187Os/188Os of whole rocks versus minerals.|
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