Different zircon recrystallization types in carbonatites caused by magma mixing: Evidence from U-Pb dating, trace element and isotope composition (Hf and O) of zircons from two Precambrian carbonatites from Fennoscandia

Chemical Geology

Volumn 353, Issue , 2013, Pages 173-198

  Tichomirowa, M ^a   Whitehouse, M J ^b   Gerdes, A ^c,d   Gotze J ^a   Schulz, B ^a   Belyatsky, B V ^e  

^a TU BERGAKADEMIE FREIBERG   (Germany)

^b SWEDISH MUSEUM OF NATURAL HISTORY   (Sweden)

^c GOETHE UNIVERSITY   (Germany)

^d STELLENBOSCH UNIVERSITY   (South Africa)

^e INSTITUTE OF PRECAMBRIAN GEOLOGY AND GEOCHRONOLOGY   (Russian Federation)

Author keywords

Carbonatites; Hf isotopes; Oxygen isotopes; U Pb; Zircons

Indexed keywords

CARBONATITES; DISSOLUTION-REPRECIPITATION; ELEVATED CONCENTRATIONS; HF ISOTOPE; ISOTOPE COMPOSITIONS; OXYGEN ISOTOPES; SOLID STATE RECRYSTALLIZATION; U-PB;

APATITE; CALCITE; CALCIUM; DIFFUSION IN LIQUIDS; GALLIUM; GEOCHEMISTRY; GEOCHRONOLOGY; HAFNIUM; IRON COMPOUNDS; ISOTOPES; LEAD; LUMINESCENCE; MICA; MIXING; OPTICAL DATA STORAGE; OPTICAL MICROSCOPY; RECRYSTALLIZATION (METALLURGY); SCANNING ELECTRON MICROSCOPY; URANIUM;

ZIRCON;

CARBONATITE; DISSOLUTION; HAFNIUM; IN SITU MEASUREMENT; INFILTRATION; ISOTOPIC COMPOSITION; MAGMA CHEMISTRY; MIXING RATIO; OXYGEN ISOTOPE; PRECAMBRIAN; PRECIPITATION (CHEMISTRY); RECRYSTALLIZATION; TRACE ELEMENT; URANIUM-LEAD DATING; ZIRCON;

FENNOSCANDIA;

EID: 84883653564     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2012.11.004     Document Type: Article

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