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

• Main Authors: Frezzotti ML, Dallai L, Sharp ZD
• Other Authors: Frezzotti, Ml, Dallai, L, Sharp, Zd
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2000
• Subjects: fluid inclusion; stable isotope; veining; metamorphic fluid; Antarctica; O'Kane Canyon; Victoria Land; Antarc*
• Online Access: http://hdl.handle.net/11573/1528743

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...