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elem24-cratons.pdf – Natural History Museum
understanding the origin of life—the Holy Grail of many a geo bioscientist. After that first summer in East Greenland, the most stun ningly beautiful place...
revmin23-moon-01-gaddis-recent-expl.pdf – Natural History Museum
m/pixel: SiO2, Al2O3, CaO, FeO, MgO, TiO2, trace elements: Th, U and K (5° × 5° or ~215 km/pixel; Ling et al. 2011; Zou et al. 2011; Wang and Niu 2012...
agu-mgr21-harquardt-mantle-conv-surf-expression.pdf – Natural History Museum
Mantle Convection and Surface Expressions Geophysical Monograph Series Geophysical Monograph Series 212 The Early Earth: Accretion and Differentiation
pnas15-badro-core-comp.pdf – Natural History Museum
2,900 km: in other words, from an evanescent thin magma ocean to a fully molten mantle, respectively. Four magma ocean geotherms span- ning the whole...
tect18-van-der-meer-seism-tomogr-slabs.pdf – Natural History Museum
Atlas of the underworld_ Slab remnants in the mantle, their sinking history, and a new outlook on lower mantle viscosity Contents lists available at S
tgeoph2-03-irifune-lm-mineralogy.pdf – Natural History Museum
combined step scan- ning and energy-dispersive measurements (Wang et al., 2004). Moreover, developments of an imaging plate (IP) detector and, more recently...
epsl04-walter-early-earth-evolution.pdf – Natural History Museum
the refractory Hf–W system [20]. Defi- ning an absolute dageT of core formation may have little real meaning for a continuous accretion process, but in...
elem05-diamond-incl-stachel.pdf – Natural History Museum
Irifune (1987) and are approximate values only. The transition zone, begin- ning at about 410 km (or 13.7 GPa) is indicated in grey. Except for crosses...