Evidence for a thick and localized ultra low shear velocity zone at the base of the mantle beneath the central Pacific

Physics of the Earth and Planetary Interiors

Volumn 184, Issue 3-4, 2011, Pages 119-133

  To, Akiko ^a   Fukao, Yoshio ^a   Tsuboi, Seiji ^a  

^a JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

Author keywords

Core mantle boundary; D" layer; Sdiff

Indexed keywords

D REGION; VELOCITY;

AZIMUTHAL VARIATIONS; CORE-MANTLE BOUNDARY; PAPUA NEW GUINEA; SDIFF; SHEAR VELOCITIES; SPECTRAL ELEMENT METHOD; STRUCTURAL MODELLING; WEAK ANOMALIES;

SHEAR FLOW;

CORE-MANTLE BOUNDARY; HETEROGENEITY; MANTLE STRUCTURE; S-WAVE; SEISMIC TOMOGRAPHY; SHEAR FLOW; THREE-DIMENSIONAL MODELING; VELOCITY STRUCTURE; WAVEFORM ANALYSIS;

PACIFIC OCEAN; PACIFIC OCEAN (CENTRAL); PAPUA NEW GUINEA;

EID: 79952737981     PISSN: 00319201     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pepi.2010.10.015     Document Type: Article

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