Oxygen and nitrogen isotopes as tracers of fluid activities in serpentinites and metasediments during subduction
N and O isotope systematics of a suite of high-pressure (HP) and ultrahigh-pressure (UHP) metasediments of the Schistes Lustrés nappe and metaperidotites of the Erro Tobbio Massif from the Alpine-Appennine system are compared with their unmetamorphosed or hydrothermally-altered equivalent from the s...
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Veröffentlicht in: | Mineralogy and petrology 2007-09, Vol.91 (1-2), p.11-24 |
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