Garnet re-equilibration by coupled dissolution-reprecipitation: Evidence from textural, major element and oxygen isotope zoning of 'cloudy' garnet

Journal of Metamorphic Geology

Volumn 29, Issue 2, 2011, Pages 213-231

  Martin, L A J ^a   Ballevre M ^b   Boulvais, P ^b   Halfpenny, A ^c   Vanderhaeghe, O ^d   Duchene S ^e   Deloule, E ^e  

^a MACQUARIE UNIVERSITY   (Australia)

^b UNIVERSITÉ DE RENNES 1   (France)

^c AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

^d Geol Gestion Rsrc Minerales/Energe   (France)

^e CRPG CNRS   (France)

Author keywords

Coupled dissolution reprecipitation; EBSD; Garnet zoning; Oxygen isotopes; Porosity

Indexed keywords

DIFFUSION IN LIQUIDS; DISSOLUTION; ISOTOPES; METAMORPHIC ROCKS; MINERALOGY; MINERALS; OXYGEN; POROSITY; ZONING;

CHEMICAL COMPOSITIONS; DIFFUSING ELEMENTS; DISSOLUTION-REPRECIPITATION; EBSD; GARNET ZONING; INTRACRYSTALLINE DIFFUSION; OXYGEN ISOTOPE COMPOSITION; OXYGEN ISOTOPES;

GARNETS;

DISSOLUTION; FLUID INCLUSION; GARNET; GEOCHEMISTRY; GROSSULAR; ISOTOPIC COMPOSITION; OXYGEN ISOTOPE; P-T CONDITIONS; P-T-T PATH; PHASE EQUILIBRIUM; POROSITY; PRECIPITATION (CHEMISTRY); PROGRADE METAMORPHISM; RETROGRADE METAMORPHISM; TEXTURE; TRACE ELEMENT; ZONING;

GREECE; IKARIA; NORTHERN AEGEAN;

EID: 79551480296     PISSN: 02634929     EISSN: 15251314     Source Type: Journal    
DOI: 10.1111/j.1525-1314.2010.00912.x     Document Type: Article

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