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Effects of an endothermic phase transition at 670 km depth in a spherical model of convection in the Earth's mantle

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Effects of an endothermic phase transition at 670 km depth in a spherical model of convection in the Earth's mantle (English)

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3

Gary A. Glatzmaier

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Paul J Tackley

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Paul J. Tackley

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David J. Stevenson

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Gerald Schubert

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language of work or name

English

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publication date

February 1993

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Nature

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volume

361

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issue

6414

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page(s)

699-704

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Development of diapiric structures in the upper mantle due to phase transitions

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7 January 2021

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Intermittent layered convection in a model mantle with an endothermic phase change at 670 km

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Chaotic, subduction-like downflows in a spherical model of convection in the Earth's mantle

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Three-Dimensional Spherical Models of Convection in the Earth's Mantle.

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Long-wavelengthS-wave velocity structure throughout the mantle

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Predominance of long-wavelength heterogeneity in the mantle

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Deep origin of mid-ocean-ridge seismic velocity anomalies

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Postspinel transformations in the system Mg2SiO4-Fe2SiO4and some geophysical implications

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Global mapping of topography on the 660-km discontinuity

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Preliminary reference Earth model

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Negative Pressure-Temperature Slopes for Reactions Formign MgSiO3 Perovskite from Calorimetry

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Parameterized mantle convection and the Earth's thermal history

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The dependence of convection planform on mode of heating

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Seismic observation of a high-velocity slab 1200-1600 km in depth

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Search for deep slabs in the Northwest Pacific mantle

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Tomographic imaging of subducted lithosphere below northwest Pacific island arcs

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Subducting slabs stagnant in the mantle transition zone

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Role of the lithosphere in mantle convection

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Large-scale mantle convection and the aggregation and dispersal of supercontinents

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Catastrophic overturn of the Earth's mantle driven by multiple phase changes and internal heat generation

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10.1038/361699A0

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1030971940

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(Q59056430)

Effects of an endothermic phase transition at 670 km depth in a spherical model of convection in the Earth's mantle

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