Seismic constraints on mantle flow and topography of the 660-km discontinuity: evidence for whole-mantle convection
- 1 October 1993
- journal article
- research article
- Published by Springer Nature in Nature
- Vol. 365 (6446) , 506-511
- https://doi.org/10.1038/365506a0
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- Three-Dimensional Instabilities of Mantle Convection with Multiple Phase TransitionsScience, 1993
- Effects of an endothermic phase transition at 670 km depth in a spherical model of convection in the Earth's mantleNature, 1993
- Subducting slabs stagnant in the mantle transition zoneJournal of Geophysical Research, 1992
- Mantle phase transitions and layered chaotic convectionGeophysical Research Letters, 1992
- Tomographic imaging of subducted lithosphere below northwest Pacific island arcsNature, 1991
- Intermittent layered convection in a model mantle with an endothermic phase change at 670 kmNature, 1991
- The large-scale structure of convection in the Earth's mantleNature, 1990
- Magma genesis, plate tectonics, and chemical differentiation of the EarthReviews of Geophysics, 1988
- Deep Slabs, Geochemical Heterogeneity, and the Large-Scale Structure of Mantle Convection: Investigation of an Enduring ParadoxAnnual Review of Earth and Planetary Sciences, 1988
- Slab penetration into the lower mantle beneath the Mariana and other island arcs of the northwest PacificJournal of Geophysical Research, 1986