Structure and composition of the subcontinental lithospheric mantle beneath the Sangilen Plateau (Tuva, southern Siberia, Russia): Evidence from lamprophyre-hosted spinel peridotite xenoliths

Lithos

Volumn 146-147, Issue , 2012, Pages 253-263

  Konc, Zoltán ^a   Marchesi, Claudio ^a   Hidas, Károly ^a   Garrido, Carlos J ^a   Szabó, Csaba ^b   Sharygin, Victor V ^c  

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

^b EÖTVÖS LORÁND UNIVERSITY   (Hungary)

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

Author keywords

Mantle metasomatism; Partial melting; Sangilen Plateau; Siberia; Spinel peridotite; Subcontinental mantle xenoliths

Indexed keywords

ACCRETION; CLINOPYROXENE; CRATON; LAMPROPHYRE; LHERZOLITE; LITHOSPHERIC STRUCTURE; MANTLE STRUCTURE; MELTING; METASOMATISM; OLIVINE; OROGENIC BELT; PARTIAL MELTING; PERIDOTITE; RARE EARTH ELEMENT; SPINEL; TRACE ELEMENT; XENOLITH;

CENTRAL ASIA; RUSSIAN FEDERATION; SIBERIA; TUVA;

EID: 84862215636     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2012.05.012     Document Type: Article

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