Persistence of mantle lithospheric Re-Os signature during asthenospherization of the subcontinental lithospheric mantle: Insights from in situ isotopic analysis of sulfides from the Ronda peridotite (Southern Spain)

Contributions to Mineralogy and Petrology

Volumn 159, Issue 3, 2010, Pages 315-330

  Marchesi, Claudio ^a,b   Griffin, William L ^b   Garrido, Carlos J ^c   Bodinier, Jean Louis ^a   O'Reilly, Suzanne Y ^b   Pearson, Norman J ^b  

^a UNIVERSITÉ MONTPELLIER 2   (France)

^b MACQUARIE UNIVERSITY   (Australia)

^c INSTITUTO ANDALUZ DE CIENCIAS DE LA TIERRA   (Spain)

Author keywords

Partial melting; Proterozoic; Re Os isotopes; Ronda massif; Subcontinental lithospheric mantle; Sulfide

Indexed keywords

AGE DETERMINATION; ASTHENOSPHERE; CONTINENTAL CRUST; CONTINENTAL LITHOSPHERE; EMPLACEMENT; GEOCHEMISTRY; GONDWANA; ISOTOPIC ANALYSIS; MANTLE STRUCTURE; OSMIUM ISOTOPE; PARTIAL MELTING; PERIDOTITE; PROTEROZOIC; RADIOMETRIC METHOD; RECRYSTALLIZATION; RHENIUM; SULFIDE; UPWELLING;

ANDALUCIA; BETIC CORDILLERA; CENTRAL EUROPE; RONDA MASSIF; SPAIN; WESTERN EUROPE;

EID: 80052296465     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-009-0429-y     Document Type: Article

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