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1.- DO RECYCLED SERPENTINITES CONTRIBUTE TO SUBDUCTION ZONE VOLCANISM? A VOTE FROM OXYGEN ISOTOPE COMPOSITIONS OF CENTRAL AMERICAN ARC LAVAS
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002
AGU 2002 FALL MEETING
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2.- OXYGEN ISOTOPE CONSTRAINTS ON THE SOURCES OF CENTRAL AMERICAN ARC LAVAS
AMERICAN GEOPHYSICAL UNION AND THE GEOCHEMICAL SOCIETY;; USA; UNITED STATES, 2005
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3.- RAPID UPLIFT OF THE ALTIPLANO REVEALED THROUGH (SUPER 13) C- (SUPER 18) O BONDS IN PALEOSOL CARBONATES
AMERICAN ASSOCIATION FOR THE ADVANCEMENT OF SCIENCE; WASHINGTON, DC; USA; UNITED STATES, 2006
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