Titre du document / Document title
Large cold anomalies in the deep mantle and mantle instability in the Cretaceous
Auteur(s) / Author(s)
YUEN D. A.
(1) ;
CADEK O. P. ;
BOEHLER R. ;
MOSER J. ;
MATYSKA C. ;
Affiliation(s) du ou des auteurs / Author(s) Affiliation(s)
(1) Univ. Minnesota, dep. geology geophysics, Minnesota supercomputer inst., Minneapolis MN 55415-1227, ETATS-UNIS
Résumé / Abstract
Two large cold masses in the deep mantle have been delineated by using long-wavelength seismic tomographic models in conjunction with mineralogical experimental data at high pressure. These cold anomalies are found under the western Pacific and the Americas with temperatures more than 1000 degrees below the ambient mantle temperature. These strong cold anomalies existing in the lower mantle today would suggest that there might have existed not too long ago a substantial temperature lump across a thermal boundary layer between the upper and lower mantle. Numerical simulations in an axisymmetric spherical-shell model incorporating the two major phase transitions have shown that very large pools of cold material with temperatures of around 1500 K can be flushed down to the coremantle boundary during this tumultuous gravitational instability
Revue / Journal Title
Terra nova
ISSN 0954-4879
Source / Source
1994, vol. 6, n
o3, pp. 238-245 (49 ref.)
Langue / Language
Anglais
Editeur / Publisher
Blackwell, Oxford, ROYAUME-UNI
(1989)
(Revue)
Mots-clés anglais / English Keywords
Cretaceous ;
mantle ;
instability ;
models ;
wavelength ;
tomography ;
thermal anomalies ;
West Pacific ;
America ;
digital simulation ;
phase transitions ;
correlation ;
subduction ;
transition zones ;
convection ;
Mesozoic ;
Pacific Ocean ;
Mots-clés français / French Keywords
Crétacé ;
Manteau ;
Instabilité ;
Modèle ;
Longueur onde ;
Tomographie ;
Anomalie thermique ;
Pacifique Ouest ;
Amérique ;
Simulation numérique ;
Transition phase ;
Corrélation ;
Subduction ;
Zone transition ;
Convection ;
Secondaire ;
Océan Pacifique ;
Mots-clés espagnols / Spanish Keywords
Cretáceo ;
Abrigo ;
Modelo ;
Tomografía ;
Anomalía termal ;
Pacífico Oeste ;
America ;
Simulación numérica ;
Transición fase ;
Correlación ;
Subducción ;
Zona transición ;
Convección ;
Secundario ;
Océano Pacífico ;
Localisation / Location
INIST-CNRS, Cote INIST : 19534 A, 35400004024379.0020
Nº notice refdoc (ud4) : 4272545