Results 231 to 240 of about 724,346 (300)

Observed Latitudinal, Longitudinal and Temporal Variability of Io's Atmosphere Simulated by a Purely Sublimation Driven Atmosphere

open access: yesJournal of Geophysical Research: Planets, Volume 130, Issue 7, July 2025.
Abstract How much of Io's SO2 ${\text{SO}}_{2}$ atmosphere is driven by volcanic outgassing or sublimation of SO2 ${\text{SO}}_{2}$ surface frost is a question with a considerable history. We develop a time dependent surface temperature model including thermal inertia and the exact celestial geometry to model the radiation driven global structure and ...
A.‐C. Dott   +5 more
wiley   +1 more source

The return of stagnant slab recorded by intraplate volcanism. [PDF]

open access: yesProc Natl Acad Sci U S A
Zhou ZB   +7 more
europepmc   +1 more source

Near Steady Late Pleistocene Tropical Denudation Rates in SW Madagascar

open access: yesJournal of Geophysical Research: Earth Surface, Volume 130, Issue 7, July 2025.
Abstract Denudation is a key parameter controlling the evolution of the Earth's surface, the production of soils, the stability of relief, or the long‐term evolution of climate. Climate fluctuations conversely have a strong impact on denudation, but these complex feedback mechanisms are still under‐constrained.
Etienne Large   +12 more
wiley   +1 more source

Crustal to mantle melt storage during the evolution of Hawaiian volcanoes. [PDF]

open access: yesSci Adv
Gazel E   +5 more
europepmc   +1 more source

Halogen abundance evidence for the formation and metasomatism of the primary lunar crust. [PDF]

open access: yesNat Commun
Jing JJ   +4 more
europepmc   +1 more source

Cosmogenic helium signatures at Deception Island volcano (Antarctica): geochronological implications for its eruptive history. [PDF]

open access: yesSci Rep
Álvarez-Valero AM   +14 more
europepmc   +1 more source

Lunar farside volcanism 2.8 billion years ago from Chang'e-6 basalts. [PDF]

open access: yesNature
Zhang QWL   +12 more
europepmc   +1 more source
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Diamonds and the Geology of Mantle Carbon

Reviews in Mineralogy and Geochemistry, 2013
### Introduction Earth’s carbon, derived from planetesimals in the 1 AU region during accretion of the Solar System, still retains similarities to carbon found in meteorites (Marty et al. 2013) even after 4.57 billion years of geological processing.
Shirey, Steven B.   +8 more
openaire   +4 more sources

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