Thermal structure of continental upper mantle inferred from S-wave velocity and surface heat flow
- 1 September 2000
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 181 (3) , 395-407
- https://doi.org/10.1016/s0012-821x(00)00209-0
Abstract
No abstract availableKeywords
This publication has 46 references indexed in Scilit:
- Eastern Asia and the Western Pacific timing and spatial distribution of rifting in ChinaPublished by Elsevier ,2003
- A xenolith-derived geotherm for southeastern australia and its geophysical implicationsPublished by Elsevier ,2003
- On the regional variation of heat flow, geotherms, and lithospheric thicknessPublished by Elsevier ,2003
- Stability and growth of continental shields in mantle convection models including recurrent melt productionTectonophysics, 1998
- Upper mantle temperatures from teleseismic tomography of French Massif Central including effects of composition, mineral reactions, anharmonicity, anelasticity and partial meltEarth and Planetary Science Letters, 1996
- Nature and composition of the continental crust: A lower crustal perspectiveReviews of Geophysics, 1995
- Lithosphere, asthenosphere, and perisphereReviews of Geophysics, 1995
- The influence of second-scale convection on the thickness of continental lithosphere and crustTectonophysics, 1991
- Shear modulus and Q of forsterite and dunite near partial melting from forced-oscillation experimentsPhysics of the Earth and Planetary Interiors, 1982
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981