Upper mantle flow in the western Mediterranean (Articolo in rivista)

Type

• Prodotto della ricerca (Classe)
• Articolo in rivista (Classe)

Label

• Upper mantle flow in the western Mediterranean (Articolo in rivista) (literal)

Anno

• 2007-01-01T00:00:00+01:00 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi

• 10.1016/j.epsl.2007.02.032 (literal)

Alternative label

• Panza G., Raykova R.B., Carminati E., Doglioni C. (2007)
  Upper mantle flow in the western Mediterranean
  in Earth and planetary science letters
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• Panza G., Raykova R.B., Carminati E., Doglioni C. (literal)

Pagina inizio

• 200 (literal)

Pagina fine

• 214 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 257 (literal)

Rivista

• Earth and planetary science letters (Rivista)

Note

• Scopu (literal)
• ISI Web of Science (WOS) (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni

• Carminati E., Doglioni C. - Dipartimento di Scienze della Terra, Università La Sapienza, Roma, Italy Panza G. - Dipartimento di Scienze della Terra, Università degli Studi di Trieste, Trieste, Italy Raykova R.B. - Geophysical Institute of BAS, Sofia, Bulgaria (literal)

Titolo

• Upper mantle flow in the western Mediterranean (literal)

Abstract

• Two cross-sections of the western Mediterranean Neogene-to-present back-arc basin are presented, in which geological and geophysical data of the TRANSMED Project are tied to a new shear-wave tomography. Major results are i) the presence of a well stratified upper mantle beneath the older African continent, with a marked low-velocity layer between 130-200 km of depth; ii) the dilution of this layer within the younger western Mediterranean back-arc basin to the north, and iii) the easterly raising of a shallower low-velocity layer from about 140 km to about 30 km in the Tyrrhenian active part of the back-arc basin. These findings suggest upper mantle circulation in the western Mediterranean back-arc basin, mostly easterly-directed and affecting the boundary between upper asthenosphere (LVZ) and lower asthenosphere, which undulates between about 180 km and 280 km. © 2007 Elsevier B.V. All rights reserved. (literal)

Prodotto di

• Institute of environmental geology and geoengineering (IGAG) (Istituto)
• Struttura crostale ed evoluzione geodinamica dell'area mediterranea (TA.P05.025.008) (Modulo)

Autore CNR

• EUGENIO AMBROGIO MARIA CARMINATI (Persona)
• CARLO DOGLIONI (Persona)

Incoming links:

Prodotto

• Institute of environmental geology and geoengineering (IGAG) (Istituto)
• Struttura crostale ed evoluzione geodinamica dell'area mediterranea (TA.P05.025.008) (Modulo)

Autore CNR di

• EUGENIO AMBROGIO MARIA CARMINATI (Persona)
• CARLO DOGLIONI (Persona)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• Earth and planetary science letters (Rivista)