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Isabella D'Este, in 1496, beseeched her agent for "black cloth for a mantle, such as shall be without a rival in the world, even if it costs 10 ducats a yard".
These results suggest that disequilibrium fluid transport in the wedge mantle, such as through channels, plays an important role in element cycling in subduction zones.
Although variable among different groups, the inferred S abundance of up to 120 ppm in the lunar mantle falls near the lower end of the S content of the depleted terrestrial mantle such as the MORB source.
(2) Would anisotropy be compatible with the NoMelt observation and, if so, what constraints can we place on the properties of the mantle such as shearing, hydration, and thermal structure?
In contrast, there is the construction in which the stem is not intended to be bonded to the cement, but rather to act as a "loaded taper" that is constrained by its surrounding cement mantle, such as the Exeter stem.
In the Fe core-silicate mantle model, shock processing that removes only the mantle, such as shocks with velocities below 100 km s−1, will preferentially return C, Si and Mg to the gas phase as compared to Fe by thermal sputtering (Fig. 6).
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Na and OH in pyrope garnet from the Colorado Plateau indicate not only UHP conditions of upper mantle origin, but also have important implications for the history of mantle metasomatism related to mantle dynamics, such as plume tectonics and subduction of oceanic plates underneath the North American Plate.
We discuss mantle overturn and accretion models that invoke episodic activity of large mantle plumes and accretion of juvenile mantle material (such as the oceanic plateaus) to the continents (the "MOMO model"), alternative arc-tectonic models, or recent suggestions for continents preservation models.
Hot lower mantle features, such as the thermal footprint of a giant impact or hot mantle plumes, will locally reduce the heat flux through the core mantle boundary (CMB), thereby weakening core convection and affecting the magnetic field generation process.
Consequently, coexisting mantle phases such as olivine and orthopyroxene should have unusually high X Mg values.
Hot mantle features, such as convective upwellings, thermal footprints of giant impacts, or chemical heterogeneities, locally reduce the heat flux through the CMB (e.g., Roberts and Zhong 2006, Roberts et al. 2009).
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