Present-day dynamic topography and lower-mantle structure from palaeogeographically constrained mantle flow models

被引:31
|
作者
Flament, Nicolas [1 ]
机构
[1] Univ Wollongong, Sch Earth & Environm Sci, GeoQuEST Res Ctr, Northfields Ave, Wollongong, NSW 2522, Australia
基金
澳大利亚研究理事会;
关键词
Structure of the Earth; Numerical modelling; Seismic tomography; Dynamics: convection currents; and mantle plumes; Dynamics of lithosphere and mantle; Rheology: mantle; TECTONIC EVOLUTION; PLATE-TECTONICS; THERMAL EXPANSIVITY; VISCOSITY STRUCTURE; GEODYNAMIC MODEL; CLUSTER-ANALYSIS; SUBDUCTED SLABS; VERTICAL MOTION; EARTHS MANTLE; POLAR WANDER;
D O I
10.1093/gji/ggy526
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
Earth's large-scale topography and lower-mantle structure are linked to past tectonic motions and mantle flow, making it possible to gain insights in the properties of the solid Earth from time-dependent global convection models driven by tectonic reconstructions. Recent work suggests that the amplitude of residual topography, obtained by subtracting models of isostatic topography from total topography, may be up to similar to 1000 m at spherical harmonic degree two (wavelength similar to 13 300 km) and > 200 m at spherical harmonic degree 12 (wavelength similar to 3000 km). The amplitude of dynamic topography and the structure of the lower mantle predicted by time-dependent forward mantle flow models both depend on the physical assumption and on model parameters. Here, I investigate the consequence of using the Boussinesq, extended Boussinesq or truncated anelastic liquid approximation (TALA) in time-dependent flow models for predicting present-day mantle structure and dynamic topography; I characterize the sensitivity of the spectral distribution of dynamic topography amplitude to the boundary conditions and model set-up for the computation of dynamic topography; and I investigate the sensitivity of model results to parameters including the depth-and temperature dependence of viscosity, the model initial age and the density of the basal layer. Extended Boussinesq and TALA models are preferred to Boussinesq models that overpredict the volume of lower-mantle slabs and the amplitude of long-wavelength dynamic topography. The correlation between dynamic and residual topography models for spherical harmonic degrees 1-3 generally ranges between 0.4 and 0.5. The flow models better predict the geographical location of large low shear velocity provinces than that of lower-mantle slabs, which cover smaller areas in map view. I show that preserving shallow lateral viscosity variations in the computation of dynamic topography increases the amplitude of dynamic topography for wavelengths > 6000 km. Parameter trade-offs exist to fit both deep and surface constraints. The best-fitting model cases considered either a moderately dense basal layer (approximately 2 per cent denser than ambient mantle) or weak temperature- and pressure dependence of lower-mantle viscosity. The fit to present-day constraints does not significantly deteriorate when extending the reconstruction of mantle flow from 200 to 410 Ma, reflecting that seismic tomography models capture the history of mantle convection over the last 200-250 Myr, and suggesting that palaeogeographically constrained mantle flow models should be compared to time-dependent surface geological constraints.
引用
收藏
页码:2158 / 2182
页数:25
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共 31 条
  • [1] Controls on the present-day dynamic topography predicted from mantle flow models since 410 Ma
    Yang, An
    Yang, Ting
    [J]. GEOPHYSICAL JOURNAL INTERNATIONAL, 2021, 225 (03) : 1637 - 1652
  • [2] Present-dayd dynamic topography and lower mantle structure from paleogeographically-constrained mantle flow models (vol 216, pg 2158, 2019)
    Flament, Nicolas
    [J]. GEOPHYSICAL JOURNAL INTERNATIONAL, 2019, 217 (02) : 1433 - 1433
  • [3] Lower mantle structure from paleogeographically constrained dynamic Earth models
    Bower, Dan J.
    Gurnis, Michael
    Seton, Maria
    [J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2013, 14 (01): : 44 - 63
  • [4] Present day mantle structure from global mantle convection models since the Cretaceous
    Pal, Debanjan
    Ghosh, Attreyee
    [J]. GEOPHYSICAL JOURNAL INTERNATIONAL, 2024, 238 (03) : 1651 - 1675
  • [5] Mantle-circulation models with sequential data assimilation: inferring present-day mantle structure from plate-motion histories
    Bunge, HP
    Richards, MA
    Baumgardner, JR
    [J]. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 2002, 360 (1800): : 2545 - 2567
  • [6] Reconciling magma-ocean crystallization models with the present-day structure of the Earth's mantle
    Ballmer, Maxim D.
    Lourenco, Diogo L.
    Hirose, Kei
    Caracas, Razvan
    Nomura, Ryuichi
    [J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2017, 18 (07): : 2785 - 2806
  • [7] Influence of past and present-day plate motions on spherical models of mantle convection: implications for mantle plumes and hotspots
    Quere, Sandrine
    Forte, Alessandro M.
    [J]. GEOPHYSICAL JOURNAL INTERNATIONAL, 2006, 165 (03) : 1041 - 1057
  • [8] MANTLE RHEOLOGY AND SATELLITE SIGNATURES FROM PRESENT-DAY GLACIAL FORCINGS
    SABADINI, R
    YUEN, DA
    GASPERINI, P
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1988, 93 (B1): : 437 - 447
  • [9] Three-dimensional visualization of numerically simulated, present-day global mantle flow
    Yoshida, Masaki
    [J]. JOURNAL OF VISUALIZATION, 2013, 16 (02) : 163 - 171
  • [10] Three-dimensional visualization of numerically simulated, present-day global mantle flow
    Masaki Yoshida
    [J]. Journal of Visualization, 2013, 16 : 163 - 171