Ion microprobe study of marble from Naxos, Greece: Grain-scale fluid pathways and stable isotope equilibration during metamorphism

Geology

Volumn 26, Issue 10, 1998, Pages 935-938

  Lewis, Stephanie ^a  

^a UNIVERSITY OF EDINBURGH   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

FLOW OF FLUIDS; GRAIN BOUNDARIES; INFILTRATION; ION MICROSCOPES; ISOTOPES; MANGANESE REMOVAL (WATER TREATMENT); MARBLE; TRACE ELEMENTS;

CATHODOLUMINESCENCE IMAGING; INFILTRATION MECHANISMS; ION MICROPROBE ANALYSIS; METAMORPHIC FLUIDS; OBSERVATIONS AND MEASUREMENTS; REALISTIC MODEL; SIMPLIFYING ASSUMPTIONS; STABLE-ISOTOPE ANALYSIS;

TRANSPORT PROPERTIES;

FLUID FLOW; GRAIN BOUNDARY; HYDROTHERMAL FLUID; MARBLE; METAMORPHISM; STABLE ISOTOPE;

GREECE; NAXOS;

EID: 84879883415     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(1998)026<0935:IMSOMF>2.3.CO;2     Document Type: Article

References (3)

1. Baker, J., 1990, Petrological and isotopic constraints on metamorphism and metamorphic fluid flow on Naxos, Greece [Ph.D. thesis]: Cambridge, University of Cambridge, 293 p.
2. Baker, J., Bickle, M. J., Buick, I. S., Holland, T. J. B., and Matthews, A., 1989, Isotopic and petrological evidence for the infiltration of water-rich fluids during the Miocene M2 metamorphism on Naxos, Greece: Geochimica et Cosmochimica Acta, v. 53, p. 2037-2050.
3. Baker, J., and Spiegelman, M., 1995, Modelling an infiltration-driven geochemical front: Earth and Planetary Science Letters, v. 136, p. 87-96.