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at least 40 km deep with limited lithospheric storage, and (2) syenites crystallized only in the sills, ∼ 1 km below the surface . San Rafael mafic magma was emplaced in sills and started to crystallize inward ...
]. The popular graphene features super-high theoretical surface area (∼2630 m2g− 1 ) and exceptional room-temperature electron mobility (∼2.5 × 105 cm2V−1s− 1 ), which allows large interfacial lithium storage ...
data and interpret the presence of low-velocity anomalies in the upper mantle as CP linked to the presence of volatile-rich melts or hydrous mineral phases . A model is then proposed for the generation ...
molecular weight and hence lower vapor pressure tend to be more enriched in fine fractions than in coarse fractions [15–17]. Coarse and fine particles dominate the dry and wet deposition fluxes ...
geochemically based calculations as well as phase equilibria (experimental and by thermodynamic modeling ) constraints imply that in excess of 50% crystallization of ultramafic rocks from initial, mantle-derived ...
abundance in mafic magmas and on S partitioning between fluid and melt phases (DSfluid/melt). The observed DSfluid/melt value increases from 51 ± 4 to 146 ± 6 when fO2 decreases from NNO + 1 ·7 ± 0·5 to NNO ...
the primary magmas to the basaltic parent magmas. Stalling of the basaltic parent magmas in the upper crust could have been controlled by the occurrence of a major crustal discontinuity, by vapor saturation ...
on an area basis (mol m–2 s– 1 ) NEE Net ecosystem exchange A measure of the net flux of carbon between the land surface and the atmosphere NSCs Non-structural carbohydrates Soluble sugars and starch ...
PLENARY LECTURES Plenary 1 : Mechanisms underling smell and stress in mammals Linda Buck Fred Hutchinson Cancer Research Center, USA, Seattle, United States The sense of smell allows mammals ...
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