Thermal state, oxygen fugacity and C-O-H fluid speciation in cratonic lithospheric mantle: New data on peridotite xenoliths from the Udachnaya kimberlite, Siberia

Earth and Planetary Science Letters

Volumn 357-358, Issue , 2012, Pages 99-110

  Goncharov, A G ^a,b,c   Ionov, D A ^a,b   Doucet, L S ^a,b   Pokhilenko, L N ^d  

^a UNIVERSITÉ DE LYON   (France)

^b UMR6524 CNRS   (France)

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

^d SOBOLEV INSTITUTE OF GEOLOGY AND MINERALOGY   (Russian Federation)

Author keywords

Geotherm; Lithospheric mantle; Metasomatism; Oxygen fugacity; Siberian craton

Indexed keywords

GEOTHERMS; LITHOSPHERIC MANTLE; METASOMATISM; OXYGEN FUGACITY; SIBERIAN CRATON;

ESTIMATION; GAS CHROMATOGRAPHY; MINERALOGY; PRESSURE EFFECTS; STRUCTURAL GEOLOGY; UNCERTAINTY ANALYSIS; YTTERBIUM;

GARNETS;

CRUST-MANTLE BOUNDARY; FUGACITY; GARNET; GAS CHROMATOGRAPHY; KIMBERLITE; LITHOSPHERIC STRUCTURE; MANTLE STRUCTURE; METASOMATISM; MOSSBAUER SPECTROSCOPY; OXYGEN; P-T CONDITIONS; PERIDOTITE; RARE EARTH ELEMENT; REDOX CONDITIONS; TEMPERATURE GRADIENT; XENOLITH;

RUSSIAN FEDERATION; SAKHA; SIBERIAN CRATON; UDACHNAYA PIPE;

EID: 84867580333     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.09.016     Document Type: Article

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