Melt infiltration of the lower lithosphere beneath the Tanzania craton and the Albertine rift inferred from S receiver functions

Geochemistry, Geophysics, Geosystems

Volumn 13, Issue 1, 2012, Pages

  Wölbern, Ingo ^a   Rümpker, Georg ^a   Link, Klemens ^b   Sodoudi, Forough ^c,d  

^a GOETHE UNIVERSITY   (Germany)

^b JOHANNES GUTENBERG UNIVERSITY   (Germany)

^c GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

^d FREIE UNIVERSITÄT BERLIN   (Germany)

Author keywords

East African Rift; lithosphere; mantle metasomatism; Tanzania craton

Indexed keywords

GEOLOGIC MODELS; MICA; MINERALOGY; SHEAR WAVES;

DENSE SYSTEMS; EAST AFRICA; EAST AFRICAN RIFT; LITHOSPHERE; LITHOSPHERE-ASTHENOSPHERE BOUNDARY; MANTLE METASOMATISM; MELT INFILTRATION; MINERAL ASSEMBLAGE; S VELOCITY; S-RECEIVER FUNCTIONS; S-WAVE VELOCITY; SEISMIC INVESTIGATIONS; SHEAR WAVE VELOCITY; TANZANIA; UPPER BOUNDARY; VELOCITY DROPS; WAVE FORMS;

VELOCITY;

ASTHENOSPHERE; DISCONTINUITY; LITHOSPHERE; MANTLE STRUCTURE; MELT; METASOMATISM; PHLOGOPITE; PYROXENITE; S-WAVE; SEISMIC VELOCITY; WAVE VELOCITY; WAVEFORM ANALYSIS; XENOLITH;

EAST AFRICAN RIFT; TANZANIA CRATON; WESTERN RIFT;

EID: 84864680418     PISSN: None     EISSN: 15252027     Source Type: Journal    
DOI: 10.1029/2012GC004167     Document Type: Article

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