The lead isotope systematics of ophiolite complexes
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Melt extraction and enrichment processes in the New Caledonia lherzolites: Evidence from geochemical and Sr-Nd isotope data
2016, LithosCitation Excerpt :Although the New Caledonia mantle bodies have been the subject of several petrological and geochemical investigations starting from the 1980s (Dupuy et al., 1981; Nicolas and Dupuy, 1984; Prinzhofer and Allegre, 1985; Prinzhofer et al., 1980), the ultra-depleted nature of these rocks hampered their geochemical characterisation. In particular, isotopic data for the peridotites are still lacking, save for some Pb isotope data (Hamelin et al., 1984). Over the past decade, several petrological and geochemical investigations were undertaken, with a view to understanding the origin of the harzburgites and associated intrusive rocks (Marchesi et al., 2009; Pirard et al., 2013; Ulrich et al., 2010).
A MORB source for low-Ti magmatism in the Semail ophiolite
2006, Chemical GeologyCitation Excerpt :Conversely, the present data set is very restricted and favors a Pb isotope homogeneous reservoir at the origin of the two types of lavas. This feature differs from results obtained on the Semail plutonic rocks (Chen and Pallister, 1981; Hamelin et al., 1984; Benoit, 1997) which underlined the large scatter shown by Pb isotopic compositions of Semail samples. The Geotimes and Lasail restricted field overlaps the field of the gabbros corresponding to the less radiogenic member of the ophiolite (Fig. 7).
Pb-isotope systematics of a fossil hydrothermal system from the Troodos ophiolite, Cyprus: Evidence for a polyphased alteration history
2000, Geochimica et Cosmochimica Acta