Results 141 to 150 of about 35,082 (263)
Abstract Throughout Gale crater on Mars, the Curiosity rover has found high abundances (15–73 wt%) of X‐ray amorphous materials in the rocks and sediments. The composition of this amorphous fraction is primarily calculated by subtracting crystalline abundances measured by the Chemistry & Mineralogy X‐Ray Diffractometer (CheMin) from bulk elemental ...
R. J. Hopkins, A. D. Rogers, L. Ehm
wiley +1 more source
Ultrahigh-energy gamma-ray emission associated with black hole-jet systems. [PDF]
Cao Z +316 more
europepmc +1 more source
A Global Prospective of the Indian Optical and Near-Infrared Observational Facilities in the Field of Astronomy and Astrophysics: a review [PDF]
Sagar, Ram
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A REVIEW OF MACHINE LEARNING APPLICATIONS IN ASTRONOMY AND ASTROPHYSICS
S.A. Shomshekova
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Abstract We investigate CO2 ${\text{CO}}_{2}$ supersaturation in the Martian southern polar night using rederived vertical profiles from Mars Global Surveyor (MGS) radio occultation (RO) measurements. Supersaturation, which affects not only local condensation but also the polar and global atmospheric dynamics, occurs when temperatures fall below the ...
Katsuyuki Noguchi +2 more
wiley +1 more source
Detection of disk-jet coprecession in a tidal disruption event. [PDF]
Wang Y +48 more
europepmc +1 more source
Astronomy and Astrophysics Hathi Trust holdings
Jeremy Guillette +2 more
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Ozone Production by Electron Irradiation of Regolith Ice: Laboratory Study for the Icy Moons
Abstract We irradiate fine‐grained regolith pure water ice in ultra high vacuum with 5keV $5\,\text{keV}$ and 10keV $10\,\text{keV}$ electrons to study the radiolysis of water ice. The ice regolith is designed to closely mimic the physical characteristics of the surfaces of the icy moons of the Solar System.
Lorenzo Obersnel +4 more
wiley +1 more source
CrossDI: A comprehensive dataset crossing three databases for calculating disruption indexes. [PDF]
Xu S, Wang C, An X, Liu J.
europepmc +1 more source
Abstract The formation of gullies on Mars has often been attributed to the melting of (sub)surface water ice. However, melting‐based hypotheses generally overlook key processes: (a) sublimation cooling by latent heat absorption, (b) the non‐stability of ice where melting conditions can be reached, and (c) the particular microclimates of gullied slopes.
L. Lange, F. Forget
wiley +1 more source

