Subsurface structure of the Solfatara volcano (Campi Flegrei caldera, Italy) as deduced from joint seismic-noise array, volcanological and morphostructural analysis

Geochemistry, Geophysics, Geosystems

Volumn 13, Issue 7, 2012, Pages

  Petrosino, Simona ^a   Damiano, Norma ^b   Cusano, Paola ^a   Di Vito, Mauro Antonio ^a   De Vita, Sandro ^a   Del Pezzo, Edoardo ^a,c  

^a OSSERVATORIO VESUVIANO   (Italy)

^b UNIVERSITY OF NAPLES FEDERICO II   (Italy)

^c UNIVERSITY OF GRANADA   (Spain)

Author keywords

Crustal structure; Seismic noise; Solfatara

Indexed keywords

ACOUSTIC WAVE VELOCITY; LITHOLOGY; POLARIZATION; SHEAR WAVES; STRUCTURAL GEOLOGY; SURFACE WAVES; VOLCANOES;

AMBIENT NOISE; ATMOSPHERIC AGENTS; CAMPI FLEGREI; CRUSTAL STRUCTURE; ERUPTIVE VENTS; FRACTURE SYSTEMS; GROUND DEFORMATIONS; HORIZONTAL-TO-VERTICAL SPECTRAL RATIOS; HYDROTHERMAL ACTIVITY; PEAK AMPLITUDE; POLARIZATION ANALYSIS; POLARIZATION PATTERNS; POLARIZATION PROPERTIES; RESONANCE FREQUENCIES; SEISMIC NOISE; SEISMIC NOISE ANALYSIS; SHEAR WAVE VELOCITY; SOLFATARA; STRUCTURAL SETTING; SUBSURFACE STRUCTURES; SURFACE WAVE DISPERSION; VARIABLE THICKNESS; VELOCITY STRUCTURE; VOLCANIC EDIFICE;

SEISMOLOGY;

AMBIENT NOISE; CALDERA; CRUSTAL STRUCTURE; DEFORMATION; GEOPHYSICAL ARRAY; HYDROTHERMAL ACTIVITY; MORPHOSTRUCTURE; POLARIZATION; S-WAVE; SEISMIC NOISE; SEISMOLOGY; SPECTRAL ANALYSIS; VOLCANIC ERUPTION; VOLCANO; VOLCANOLOGY; WAVE DISPERSION; WAVE PROPAGATION; WAVE VELOCITY;

CAMPANIA [ITALY]; ITALY; NAPOLI [CAMPANIA]; SOLFATARA;

EID: 84864072955     PISSN: None     EISSN: 15252027     Source Type: Journal    
DOI: 10.1029/2011GC004030     Document Type: Review

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