Utilize este identificador para referenciar este registo: http://hdl.handle.net/10400.21/1298
Título: Stratification of the earth beneath the Azores from P and S receiver functions
Autor: Silveira, Graça
Vinnik, Lev
Stutzmann, E.
Farra, V.
Kiselev, Sergei
Morais, Iolanda
Palavras-chave: Receiver functions
Hotspots
Mantle transition zone
Azores
Mantle structure beneath
Mid-atlantic ridge
Converted waves
Southern Africa
Rayleigh-wave
Tomography
Velocity
Iceland
Plumes
Lithosphere
Data: 15-Out-2010
Editora: Elsevier Science BV
Citação: Silveira G, Vinnik L, Stutzmann E, Farra V, Kiselev S, Morais I. Stratification of the Earth beneath the Azores from P and S receiver functions. Earth and Planetary Science Letters. 2010; 299 (1-2): 91-103.
Relatório da Série N.º: 1-2
Resumo: Seismic recordings of IRIS/IDA/GSN station CMLA and of several temporary stations in the Azores archipelago are processed with P and S receiver function (PRF and SRF) techniques. Contrary to regional seismic tomography these methods provide estimates of the absolute velocities and of the Vp/Vs ratio up to a depth of similar to 300 km. Joint inversion of PRFs and SRFs for a few data sets consistently reveals a division of the subsurface medium into four zones with a distinctly different Vp/Vs ratio: the crust similar to 20 km thick with a ratio of similar to 1.9 in the lower crust, the high-Vs mantle lid with a strongly reduced VpNs velocity ratio relative to the standard 1.8, the low-velocity zone (LVZ) with a velocity ratio of similar to 2.0, and the underlying upper-mantle layer with a standard velocity ratio. Our estimates of crustal thickness greatly exceed previous estimates (similar to 10 km). The base of the high-Vs lid (the Gutenberg discontinuity) is at a depth of-SO km. The LVZ with a reduction of S velocity of similar to 15% relative to the standard (IASP91) model is terminated at a depth of similar to 200 km. The average thickness of the mantle transition zone (TZ) is evaluated from the time difference between the S410p and SKS660p, seismic phases that are robustly detected in the S and SKS receiver functions. This thickness is practically similar to the standard IASP91 value of 250 km. and is characteristic of a large region of the North Atlantic outside the Azores plateau. Our data are indicative of a reduction of the S-wave velocity of several percent relative to the standard velocity in a depth interval from 460 to 500 km. This reduction is found in the nearest vicinities of the Azores, in the region sampled by the PRFs, but, as evidenced by SRFs, it is missing at a distance of a few hundred kilometers from the islands. We speculate that this anomaly may correspond to the source of a plume which generated the Azores hotspot. Previously, a low S velocity in this depth range was found with SRF techniques beneath a few other hotspots.
Peer review: yes
URI: http://hdl.handle.net/10400.21/1298
ISSN: 0012-821X
Aparece nas colecções:ISEL - Física - Artigos

Ficheiros deste registo:
Ficheiro Descrição TamanhoFormato 
Stratification of the Earth beneath the Azores from P and S receiver functions.rep.pdf53,12 kBAdobe PDFVer/Abrir


FacebookTwitterDeliciousLinkedInDiggGoogle BookmarksMySpace
Formato BibTex MendeleyEndnote Degois 

Todos os registos no repositório estão protegidos por leis de copyright, com todos os direitos reservados.