Journal of Petrology Advance Access originally published online on December 22, 2005
Journal of Petrology 2006 47(4):745-771; doi:10.1093/petrology/egi092
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Discontinuous Melt Extraction and Weak Refertilization of Mantle Peridotites at the Vema Lithospheric Section (Mid-Atlantic Ridge)
1 ISTITUTO DI SCIENZE MARINE, GEOLOGIA MARINA, CNR, VIA GOBETTI 101, 40129 BOLOGNA, ITALY
2 LABORATORIE P. SÜE, CEA-CNRS, BÂT. 637, GIF SUR YVETTE, 91191, FRANCE
3 LABORATOIRE DE MINÉRALOGIE–PÉTROLOGIE, UMR 7160 CNRS–MUSÉUM NATIONAL D'HISTOIRE NATURELLE, 61 RUE BUFFON, PARIS 75005, FRANCE
4 DEPARTMENT OF EARTH AND ENVIRONMENTAL SCIENCES, LAMONT DOHERTY EARTH OBSERVATORY, COLUMBIA UNIVERSITY, PALISADES, NY 10964, USA
5 ISTITUTO DI GEOSCIENZE E GEORISORSE, SEDE DI PAVIA, CNR, VIA FERRATA 1, 27100, PAVIA, ITALY
6 DIPARTIMENTO DI SCIENZE DELLA TERRA, UNIVERSITÀ ‘LA SAPIENZA’, PIAZZALE ALDO MORO 5, 00187, ROME, ITALY
RECEIVED OCTOBER 27, 2004; ACCEPTED NOVEMBER 16, 2005
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.
KEY WORDS: mantle partial melting; abyssal peridotite; trace element; refertilization; Vema Fracture Zone
* Corresponding author. Present address: Laboratoire P. Süe, CEA–CNRS, Gif sur Yvette, 91191 France. Telephone: +33 16908 9522. Fax: +33 16908 6923. E-mail: daniele.brunelli{at}bo.ismar.cnr.it
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