Enrichment of HFSE in chlorite-harzburgite produced by high-pressure dehydration of antigorite-serpentinite: Implications for subduction magmatism
Article first published online: 20 JAN 2005
Copyright 2005 by the American Geophysical Union.
Geochemistry, Geophysics, Geosystems
Volume 6, Issue 1, January 2005
How to Cite
2005), Enrichment of HFSE in chlorite-harzburgite produced by high-pressure dehydration of antigorite-serpentinite: Implications for subduction magmatism, Geochem. Geophys. Geosyst., 6, Q01J15, doi:10.1029/2004GC000791., , , , , , and (
- Issue published online: 20 JAN 2005
- Article first published online: 20 JAN 2005
- Manuscript Accepted: 19 NOV 2004
- Manuscript Revised: 29 OCT 2004
- Manuscript Received: 2 JUL 2004
Auxiliary material for this article contains a table of LA-ICP-MS and ICP-MS analyses of PH-1 clinopyroxene, a peridotite from the French Massif Central peridotite.
Additional file information is provided in the readme.txt.
|ggge586-sup-0001readme.txt||plain text document||1K||readme.txt|
|ggge586-sup-0002tab01.txt||plain text document||5K||Tab-delimited Table 1.|
|ggge586-sup-0003tab02.txt||plain text document||3K||Tab-delimited Table 2.|
|ggge586-sup-0004tab03.txt||plain text document||2K||Tab-delimited Table 3.|
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