Fluid-inclusion and stable-isotope evidence for fluid infiltration and veining during metamorphism in marbles and metapelites

• Published in: European Journal of Mineralogy
• Main Authors: Frezzotti, M, Dallai, L, Sharp, Z.
• Other Authors: Sharp, Z
• Format: Article in Journal/Newspaper
• Language: English
• Published: E. Schweizerbart'sche Verlagsbuchhandlung 2000
• Subjects: Antarctica; Fluid inclusion; Metamorphic fluid; Stable isotope; Veining; stable isotopes; petrology; GEO/07 - PETROLOGIA E PETROGRAFIA; GEO/08 - GEOCHIMICA E VULCANOLOGIA; Victoria Land; O'Kane Canyon; Antarc*
• Online Access: http://hdl.handle.net/10281/174635; https://doi.org/10.1127/ejm/12/1/0231

Syn-metamorphic quartz + carbonate veins within lower-amphibolite-facies marbles and greenschist-facies metapelites of the O'Kane Canyon (northern Victoria Land, Antarctica) are characterised by fluids of different composition: H2O-CO2-CH4 mixtures (34-44 H2O, 50-61 CO2, 3-6 CH4, in mole %) (Ty...