3SMAC: An a priori tomographic model of the upper mantle based on geophysical modeling

被引:292
作者
Nataf, HC
Ricard, Y
机构
[1] Dept. Terre-Atmosphere-Ocean, URA 1316 du CNRS, Ecl. Normale Supérieure, 75231 Paris Cedex 05
[2] Dept. de Géologie, URA 726 du CNRS, Ecl. Normale Sup. de Lyon, 69364 Lyon Cedex 07
关键词
D O I
10.1016/0031-9201(95)03105-7
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present an a priori three-dimensional 'tomographic' model of the upper mantle. We construct this model (called 3SMAC - three-dimensional seismological model a priori constrained) in four steps: we compile information on the thickness of 'chemical' layers in the Earth (water, sediments, upper and lower crust, etc); we get a 3D temperature distribution from thermal plate models applied to the oceans and continents; we deduce the mineralogy in the mantle from pressure and temperature and we finally get a three-dimensional model of density, seismic velocities, and attenuation by introducing laboratory measurements of these quantities as a function of pressure and temperature. The model is thus consistent with various geophysical data, such as ocean bathymetry, and surface heat flux. We use this model to compute synthetic travel-times of body waves, and we compare them with observations. A similar exercise is performed for surface waves and normal modes in a companion paper (Ricard et al., 1996, J. Geophys. Res., in press). We find that our model predicts the bulk of the observed travel-time variations. Both the amplitude and general pattern are well recovered. The discrepancies suggest that tomography can provide useful regional information on the thermal state of the continents. In the oceans, the flattening of the sea-floor beyond 70 Ma seems difficult to reconcile with the seismic observations. Overall, our 3SMAC model is both a realistic model, which can be used to test various tomographic methods, and a model of the minimum heterogeneities to be expected from geodynamical modeling. Therefore, it should be a useful a priori model to be used in tomographic inversions, in order to retrieve reliable images of heterogeneities in the transition zone, which should, in turn, greatly improve our understanding of geodynamical processes in the deep Earth. 3SMAC and accompanying software can be retrieved by anonymous ftp at geoscope.ipgp.jussieu.fr.
引用
收藏
页码:101 / 122
页数:22
相关论文
共 106 条
[21]  
EWING M, 1993, GEOL SOC AM BULL, V84, P71
[22]  
FIELDING EJ, 1993, GEOLOGICAL GEOPHYSIC
[23]   SHORT-WAVELENGTH GEOID, BATHYMETRY AND THE CONVECTIVE PATTERN BENEATH THE PACIFIC-OCEAN [J].
FLEITOUT, L ;
MORICEAU, C .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1992, 110 (01) :6-28
[24]   SECONDARY CONVECTION AND THE GROWTH OF THE OCEANIC LITHOSPHERE [J].
FLEITOUT, L ;
YUEN, DA .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1984, 36 :181-212
[25]   SMALL-WAVELENGTH GEOID AND TOPOGRAPHY ANOMALIES IN THE SOUTH-ATLANTIC OCEAN - A CLUE TO NEW HOT-SPOT TRACKS AND LITHOSPHERIC DEFORMATION [J].
FLEITOUT, L ;
DALLOUBEIX, C ;
MORICEAU, C .
GEOPHYSICAL RESEARCH LETTERS, 1989, 16 (07) :637-640
[26]   UPPER MANTLE SHEAR STRUCTURE OF NORTH-AMERICA [J].
GRAND, SP ;
HELMBERGER, DV .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1984, 76 (02) :399-438
[27]   MANTLE SHEAR STRUCTURE BENEATH THE AMERICA AND SURROUNDING OCEANS [J].
GRAND, SP .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1994, 99 (B6) :11591-11621
[28]   UPPER MANTLE SHEAR STRUCTURE BENEATH THE NORTHWEST ATLANTIC-OCEAN [J].
GRAND, SP ;
HELMBERGER, DV .
JOURNAL OF GEOPHYSICAL RESEARCH, 1984, 89 (NB13) :1465-1475
[29]   UPPER MANTLE CROSS-SECTION FROM TONGA TO NEWFOUNDLAND [J].
GRAVES, RW ;
HELMBERGER, DV .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1988, 93 (B5) :4701-4711
[30]   Q-1 OF FORSTERITE SINGLE-CRYSTALS [J].
GUEGUEN, Y ;
DAROT, M ;
MAZOT, P ;
WOIRGARD, J .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1989, 55 (3-4) :254-258