Evidence for retrograde lithospheric subduction on Venus [PDF]
Though there is no plate tectonics per se on Venus, recent Magellan radar images and topographic profiles of the planet suggest the occurrence of the plate tectonic processes of lithospheric subduction and back-arc spreading.
Sandwell, David T., Schubert, Gerald
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Solar X-ray and EUV imager on board the FY-3E satellite. [PDF]
Chen B +45 more
europepmc +1 more source
Mountain Belts on Venus and Earth [PDF]
Sponsored by Lunar and Planetary Institute, San Juan Capistrano Research Institute, NASA Johnson Space Centercompiled by Lunar and Planetary InstitutePARTIAL CONTENTS: Terrestrial Mountain Belts and Venusian Plateau-shaped Highlands as Manifestations of ...
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A globally fragmented and mobile lithosphere on Venus. [PDF]
Byrne PK +5 more
europepmc +1 more source
Distribution of water phase near the poles of the Moon from gravity aspects. [PDF]
Kletetschka G +5 more
europepmc +1 more source
Geochemistry and mineral chemistry of pelitic gneiss of Ikare area, southwestern Nigeria. [PDF]
Oziegbe EJ +3 more
europepmc +1 more source
The Case against Mercury as the Angrite Parent Body (APB) [PDF]
Angrites are not plausibly from Mercury based on their high FeO contents and ancient ages (e.g., [1]). Rather, the early crystallization ages of angrites argues for a small asteroidal-sized parent body for these meteorites (e.g., [2]).
Hutson, M. L. +2 more
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Elemental abundances of major elements in the solar wind as measured in Genesis targets and implications on solar wind fractionation. [PDF]
Heber VS +7 more
europepmc +1 more source
The thermosphere and ionosphere of Venus [PDF]
Our knowledge of the upper atmosphere and ionosphere of Venus and its interaction with the solar wind has advanced dramatically over the last decade, largely due to the data obtained during the Pioneer Venus mission and to the theoretical work that was ...
Cravens, T. E.
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Las hornblenditas,gabros y dioritas del Macizo del Montnegre (Barcelona, Cordilleras costero catalanas) [PDF]
En relación con los granitos tardihercínicos calcoalcalinos del Macizo del Montnegre aparecen rocas ultrabásicas-básicas a intermedias. Las más básicas son hornblenditas olivínicas, con espinela, clinopiroxeno, ortopiroxeno, anfíboles de varios tipos y ...
Butjosa Molines, Lidia +2 more
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