Evidence of a partial melt zone beneath Stromboli volcano (Italy) from inversion of teleseismic receiver functions

Terra Nova

Volumn 21, Issue 5, 2009, Pages 386-392

  Martinez Arevalo, Carmen ^a   Musumeci, Carla ^b   Patanè, Domenico ^b  

^a MUSEO NACIONAL DE CIENCIAS NATURALES   (Spain)

^b ISTITUTO NAZIONALE DI GEOFISICA E VULCANOLOGIA   (Italy)

Author keywords

[No Author keywords available]

Indexed keywords

ALGORITHM; BODY WAVE; DISCONTINUITY; ESTIMATION METHOD; MANTLE STRUCTURE; MOHO; PARAMETERIZATION; PARTIAL MELTING; PETROLOGY; S-WAVE; SEISMIC TOMOGRAPHY; TELESEISMIC WAVE; VOLCANISM; WAVE VELOCITY;

EURASIA; EUROPE; ITALY; LIPARI ISLANDS; MESSINA [SICILY]; SICILY; SOUTHERN EUROPE; STROMBOLI;

EID: 70350102337     PISSN: 09544879     EISSN: 13653121     Source Type: Journal    
DOI: 10.1111/j.1365-3121.2009.00894.x     Document Type: Article

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