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]
Zhou ZB+7 more
europepmc +1 more source
Near Steady Late Pleistocene Tropical Denudation Rates in SW Madagascar
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
Magnetotelluric evidence for the deep causes of different eruptive styles of Changbaishan Tianchi and Longgang volcanoes. [PDF]
Zhao L+8 more
europepmc +1 more source
Crustal to mantle melt storage during the evolution of Hawaiian volcanoes. [PDF]
Gazel E+5 more
europepmc +1 more source
Halogen abundance evidence for the formation and metasomatism of the primary lunar crust. [PDF]
Jing JJ+4 more
europepmc +1 more source
Cosmogenic helium signatures at Deception Island volcano (Antarctica): geochronological implications for its eruptive history. [PDF]
Álvarez-Valero AM+14 more
europepmc +1 more source
Lunar farside volcanism 2.8 billion years ago from Chang'e-6 basalts. [PDF]
Zhang QWL+12 more
europepmc +1 more source
Sm-Nd Isotope Data Compilation from Geoscientific Literature Using an Automated Tabular Extraction Method. [PDF]
Guo Z+6 more
europepmc +1 more source
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