Garnet pyroxenite layers from the mantle peridotites of the Northern Apennine ophiolites, Italy: Evidence for recycling of crustal material?

Details Garnet pyroxenite layers from the mantle peridotites of the Northern Apennine ophiolites, Italy: Evidence for recycling of crustal material? Garnet pyroxenite layers from the mantle peridotites of the Northern Apennine ophiolites, Italy: Evidence for recycling of crustal material?

Aug 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006gecas..70r.426m&link_type=ejournal

Geochimica et Cosmochimica Acta, Volume 70, Issue 18, p. A426-A426.

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