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Detrital, metamorphic and metasomatic tourmaline in high-pressure metasediments from Syros (Greece): intra-grain boron isotope patterns determined by secondary-ion mass spectrometry
Auteur(s)
Marschall, Horst R.
Editeur(s)
Date de parution
2008
In
Contributions to Mineralogy and Petrology, Springer, 2008/155/6/703-717
Résumé
The boron isotopic composition of zoned tourmaline in two metasediments from the island of Syros, determined by secondary-ion mass spectrometry (SIMS), reflects the sedimentary and metamorphic record of the rocks. Tourmaline from a silicate-bearing marble contains small (≤20 μm) detrital cores with highly variable δ<sup>11</sup>B values (−10.7 to +3.6‰), pointing to a heterogeneous protolith derived from multiple sources. The sedimentary B isotopic record survived the entire metamorphic cycle with peak temperatures of ~500°C. Prograde to peak metamorphic rims are homogeneous and similar among all analysed grains (δ<sup>11</sup>B ≈ +0.9‰). The varying δ<sup>11</sup>B values of detrital cores in the siliceous marble demonstrate that in situ B isotope analysis of tourmaline by SIMS is a potentially powerful tool for provenance studies not only in sediments but also in metasediments. A meta-tuffitic blueschist bears abundant tourmaline with dravitic cores of detrital or authigenic origin (δ<sup>11</sup>B ≈ −3.3‰), and prograde to peak metamorphic overgrowth zones (−1.6‰). Fe-rich rims, formed during influx of B-bearing fluids under retrograde conditions, show strongly increasing δ<sup>11</sup>B values (up to +7.7‰) towards the margins of the grains. The δ<sup>11</sup>B values of metamorphic tourmaline from Syros, formed in mixed terrigenous–marine sediments, reflect the B signal blended from these two different sources, and was probably not altered by dehydration during subduction.
Autre version
http://dx.doi.org/10.1007/s00410-007-0266-9
Type de publication
Resource Types::text::journal::journal article
