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Earth and planetary science letters, ISSN 0012-821X, 01/2015, Volume 409, pp. 225 - 231
.... In the common view, this preservation is due to the fact that the thermal boundary layers are compositionally distinct from the ambient mantle in that they are highly melt-depleted and dehydrated... 
continental destabilization | lithospheric initial thickness | peridotite xenolith | refertilization | Refertilization | Peridotite xenolith | Lithospheric initial thickness | Continental destabilization | Physical Sciences | Science & Technology | Geochemistry & Geophysics | Silicates | Rocks, Igneous | Inclusions | Mines and mineral resources | Lithosphere | Boundary layer | Melting | Buoyancy | Thermal boundary layer | Continents | Positive feedback | Mantle | Melts
Journal Article
Journal of petrology, ISSN 0022-3530, 11/2006, Volume 47, Issue 11, pp. 2233 - 2256
...) and similar to 80 mW/m(2) (Neogene). Garnet peridotite xenoliths or xenocrysts from the Paleozoic kimberlites are strongly depleted, similar to peridotites from other areas of cratonic mantle, with magnesium... 
North China Craton | Mantle replacement | UHP lithosphere evolution | Sulu UHP terrane | Garnet peridotite xenoliths | Lithospheric thinning | Physical Sciences | Science & Technology | Geochemistry & Geophysics
Journal Article
Earth and planetary science letters, ISSN 0012-821X, 12/2015, Volume 432, pp. 232 - 242
.... Thus we investigate the possibility that, at geological strain-rates, these recovery processes allow steady-state deformation by dislocation creep at low to moderate temperatures in the lithospheric mantle... 
numerical modelling | creep | deformation | olivine rheology | lithospheric mantle | Lithospheric mantle | Deformation | Creep | Numerical modelling | Olivine rheology | Physical Sciences | Science & Technology | Geochemistry & Geophysics | Olivine | Stresses | Mathematical models | Creep (materials) | Mantle | Recovery | Dislocations | Earth Sciences | Sciences of the Universe | Tectonics | Environmental Sciences | Global Changes
Journal Article
Geochimica et cosmochimica acta, ISSN 0016-7037, 2010, Volume 74, Issue 1, pp. 293 - 320
Spinel lherzolite xenoliths from Mont Briançon, French Massif Central, retain evidence for multiple episodes of melt depletion and melt/fluid infiltration... 
Physical Sciences | Science & Technology | Geochemistry & Geophysics | Metasomatism (Mineralogy) | Geochronology | Peridotite | Rocks, Igneous | Environmental sciences | Spinel group | Silicates | Inclusions | Magma | Earth | Sulfides | Lime | Analysis | Age | Geochemistry | Earth Sciences | Sciences of the Universe | Environmental Sciences | Global Changes
Journal Article
Lithos, ISSN 0024-4937, 02/2014, Volume 189, pp. 2 - 15
...–Os model ages on sulfides and alloys in mantle-derived rocks and xenocrysts, to examine patterns of crustal evolution and crust... 
Lithospheric mantle Hadean zircons | Mantle Os-isotopes | Crust–mantle evolution | Hadean | Archean | Lithospheric mantle hadean zircons | Crust-mantle evolution | Physical Sciences | Mineralogy | Science & Technology | Geochemistry & Geophysics | Earth | Sulfur compounds | Mantle | Analysis | Alloys | Tectonics (Geology)
Journal Article
Geochemistry, geophysics, geosystems : G3, ISSN 1525-2027, 01/2019, Volume 20, Issue 1, pp. 183 - 207
To constrain the deformation, thermal evolution, and seismic properties of the mantle lithosphere beneath the Hangay Dome, we have analyzed the microstructures, crystal preferred orientations (CPO... 
Hangay Dome | peridotite | seismic anisotropy | CPO | hydrogen | lithospheric mantle | Physical Sciences | Science & Technology | Geochemistry & Geophysics | Olivine | Deformation | Seismic activity | Hydrogen | Lithosphere | High temperature | Magma | Physical properties | Equilibrium | Seismic properties | Garnet | Anisotropy | Seismic velocities | Evolution | Wave velocity | Cenozoic | Mantle | Basalts | Hydrogen ion concentration | Anomalies | Geochemistry | Earth Sciences | Sciences of the Universe | Geophysics
Journal Article
Geophysical Research Letters, ISSN 0094-8276, 09/2009, Volume 36, Issue 18, pp. L18203 - n/a
... or more lateral variations in both mantle heat flux and lithospheric thickness and is the preferred explanation for the polar elastic thickness measurement. Our mantle plume models, which have previously been shown to explain observations of present‐day magma production on Mars, can also explain the new elastic thickness observations. 
general | convection currents, and mantle plumes | Dynamics | Lithospheric flexure | Tectonophysics | Interiors | Planetary Sciences | Solid Surface Planets | Dynamics of lithosphere and mantle | Mars polar cap | Mars lithosphere | Mars mantle convection | Geosciences, Multidisciplinary | Physical Sciences | Geology | Science & Technology | Planets | Planetology | Plate tectonics | Continental dynamics | Polar layered deposits | Mars | Geophysics | Thickness measurements | Mantle | Convection | Heat transfer | Radioactivity
Journal Article