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Y. Sumino, O. Anderson, I. Suzuki (2013)
Temperature coefficients of elastic constants of single crystal MgO between 80 and 1,300 KPhysics and Chemistry of Minerals, 9
S. Crough (1975)
Thermal model of oceanic lithosphereNature, 256
J. Dercourt, L. Zonenshain, L. Ricou, V. Kazmin, X. Pichon, A. Knipper, C. Grandjacquet, I. Sbortshikov, J. Geyssant, C. Lepvrier, D. Pechersky, J. Boulin, J. Sibuet, L. Savostin, O. Sorokhtin, M. Westphal, M. Bazhenov, J. Lauer, B. Biju-Duval (1986)
Geological evolution of the tethys belt from the atlantic to the pamirs since the LIASTectonophysics, 123
W. Spakman (1990)
Tomographic images of the upper mantle below central Europe and the MediterraneanTerra Nova, 2
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Thermal regime of a downgoing slab and new global tectonicsJournal of Geophysical Research, 75
O. Anderson, E. Schreiber, R. Liebermann, N. Soga (1968)
Some elastic constant data on minerals relevant to geophysicsReviews of Geophysics, 6
D. Peaceman, H. Rachford (1955)
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I. Suzuki, O. Anderson, Y. Sumino (1983)
Elastic properties of a single-crystal forsterite Mg2SiO4, up to 1,200 KPhysics and Chemistry of Minerals, 10
Douglas Douglas (1955)
On the numerical integration of δ 2 u /δ x 2 +δ 2 u /δ y 2 =δ u /δ t by implicit methodsJ. Soc. Ind. Appl. Math., 3
J. Douglas (1955)
On the Numerical Integration of $\frac{\partial ^2 u}{\partial x^2 } + \frac{\partial ^2 u}{\partial y^2 } = \frac{\partial u}{\partial t}$ by Implicit MethodsJournal of The Society for Industrial and Applied Mathematics, 3
W. Spakman, M. Wortel, N. Vlaar (1988)
The Hellenic Subduction Zone: A tomographic image and its geodynamic implicationsGeophysical Research Letters, 15
Spakman Spakman (1988)
Upper mantle delay time tomography, PhD thesis, University of UtrechtGeol. Ultraiect., 53
ABSTRACT We develop and present an approach for gaining insight into the thermal structure of the upper mantle in a tectonically active region. As a starting point for the analysis we use regional geological reconstructions, based on data from surface geology, shallow seismics and paleomagnetism. For these reconstructions we determine the necessarily associated upper mantle processes, such as subduction. We then forwardly model the thermal structure of upper mantle corresponding with the geological reconstruction used. In this way we obtain an estimate of a very important characteristic – the temperature distribution of the upper mantle–that is independent from those estimates from the usual deep seismic methods. If sufficient detailed information on the seismological structure of the region is available, a quantitative test of our modelling results is possible, via the temperature dependence of seismic velocities. We apply our approach to the Mediterranean area, for which we will test the reconstruction published by Dercourt et al. (1986).
Terra Nova – Wiley
Published: Nov 1, 1990
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