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Journal of Petrology Advance Access published online on December 22, 2005

Journal of Petrology, doi:10.1093/petrology/egi092
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© The Author 2005. Published by Oxford University Press. All rights reserved. For Permissions, please e-mail: journals.permissions@oxfordjournals.org
Received October 27, 2004
Accepted November 16, 2005

Article

Discontinuous Melt Extraction and Weak Refertilization of Mantle Peridotites at the Vema Lithospheric Section (Mid-Atlantic Ridge)

DANIELE BRUNELLI 1 *, MONIQUE SEYLER 2, ANNA CIPRIANI 3, LUISA OTTOLINI 4, and ENRICO BONATTI 5

1 ISTITUTO DI SCIENZE MARINE, GEOLOGIA MARINA, CNR, VIA GOBETTI 101, 40129 BOLOGNA, ITALY; LABORATORIE P. SÜE, CEA-CNRS, BÂT. 637, GIF SUR YVETTE, 91191, FRANCE
2 LABORATOIRE DE MINÉRALOGIE-PÉTROLOGIE, UMR 7160 CNRS-MUSÉUM NATIONAL D'HISTOIRE NATURELLE, 61 RUE BUFFON, PARIS 75005, FRANCE
3 DEPARTMENT OF EARTH AND ENVIRONMENTAL SCIENCES, LAMONT DOHERTY EARTH OBSERVATORY, COLUMBIA UNIVERSITY, PALISADES, NY 10964, USA
4 ISTITUTO DI GEOSCIENZE E GEORISORSE, SEDE DI PAVIA, CNR, VIA FERRATA 1, 27100, PAVIA, ITALY
5 ISTITUTO DI SCIENZE MARINE, GEOLOGIA MARINA, CNR, VIA GOBETTI 101, 40129 BOLOGNA, ITALY; DEPARTMENT OF EARTH AND ENVIRONMENTAL SCIENCES, LAMONT DOHERTY EARTH OBSERVATORY, COLUMBIA UNIVERSITY, PALISADES, NY 10964, USA; DIPARTIMENTO DI SCIENZE DELLA TERRA, UNIVERSITÀ ‘LA SAPIENZA’, PIAZZALE ALDO MORO 5, 00187, ROME, ITALY

* To whom correspondence should be addressed.
DANIELE BRUNELLI, E-mail: daniele.brunelli{at}bo.ismar.cnr.it


   Abstract

Melting processes beneath the Mid-Atlantic Ridge were studied in residual mantle peridotites sampled from a lithospheric section exposed near the Vema Fracture Zone at 11°N along the Mid-Atlantic Ridge. Fractional and dynamic melting models were tested based on clinopyroxene rare earth element and high field strength element data. Pure fractional melting (non-modal) cannot account for the observed trends, whereas dynamic melting with critical mass porosity <0·01 fits better the measured values. Observed microtextures suggest weak refertilization with 0·1-1% quasi-instantaneous or partially aggregated melts trapped during percolation. The composition of the melts is evaluated, together with their provenance, with respect to the garnet-spinel transition. Partial melts appear to be aggregated over short but variable intervals of the melting column. Deep melts (generated within the garnet stability field at the base of the melting column) escape detection, being separated from the residues by transport inside conduits or fractures. The temporal evolution of the melting process along the exposed section shows a steady increase of mantle temperature from 20 Ma to present.

Keywords: mantle partial melting; abyssal peridotite; trace element; refertilization; Vema Fracture Zone.
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