Trace element and O-isotope composition of polyphase metamorphic veins of the Ile de Groix (Armorican Massif, France) implication for fluid flow during HP subduction and exhumation processes
ContributorsEl Korh, Afifé; Schmidt, Susanne Theodora; Vennemann, Torsten; Ulianov, Alexey
Published inDobrzhinetskaya, L., Faryard, W., Wallis, S., Cuthbert, S. (Ed.), Ultrahigh Pressure Metamorphism: 25 years after discovery of coesite and diamond, p. 243-291
PublisherAmsterdam : Elsevier
Publication date2011
Research groups
Citation (ISO format)
EL KORH, Afifé et al. Trace element and O-isotope composition of polyphase metamorphic veins of the Ile de Groix (Armorican Massif, France) implication for fluid flow during HP subduction and exhumation processes. In: Ultrahigh Pressure Metamorphism: 25 years after discovery of coesite and diamond. Dobrzhinetskaya, L., Faryard, W., Wallis, S., Cuthbert, S. (Ed.). Amsterdam : Elsevier, 2011. p. 243–291.
Identifiers
- PID : unige:29588
Additional URL for this publicationhttp://www.elsevier.com/books/ultrahigh-pressure-metamorphism/dobrzhinetskaya/978-0-12-385144-4#
ISBN978-0-12-385144-4
