Flux of carbonate melt from deeply subducted pelitic sediments: Geophysical and geochemical implications for the source of Central American volcanic arc
Version of Record online: 24 AUG 2012
©2012. American Geophysical Union. All Rights Reserved.
Geophysical Research Letters
Volume 39, Issue 16, 28 August 2012
How to Cite
2012), Flux of carbonate melt from deeply subducted pelitic sediments: Geophysical and geochemical implications for the source of Central American volcanic arc, Geophys. Res. Lett., 39, L16307, doi:10.1029/2012GL052606., , , and (
- Issue online: 24 AUG 2012
- Version of Record online: 24 AUG 2012
- Manuscript Accepted: 11 JUL 2012
- Manuscript Revised: 6 JUL 2012
- Manuscript Received: 5 JUN 2012
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|grl29472-sup-0001-readme.txt||plain text document||3K||readme.txt|
|grl29472-sup-0002-txts01.doc||Word document||219K||Text S1. Multi anvil experiments, compositions of the sedimentary starting materials, phase compositions from partial melting experiments, and jadeite and calcium-Tschermak component of clinopyroxene as a function of temperature from 5 GPa melting experiments of carbonated pelite.|
|grl29472-sup-0003-t01.txt||plain text document||4K||Tab-delimited Table 1.|
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