Results 141 to 150 of about 505 (181)
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Gravoturbulent planetesimal formation

Physica Scripta, 2008
We present a new scenario for the rapid formation of planetesimals based on the combined effects of turbulence and gravity. While it was generally accepted that these two effects cancel each other out, we found their interaction to be extremely beneficial for the accumulation of larger objects bound by gravity.
H Klahr, A Johansen
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Xenon fractionation in porous planetesimals

Geochimica et Cosmochimica Acta, 1990
The distinctively fractionated Xe on Mars and Earth may have its root in a common source from which both planets accreted. We begin with Ozima and Nakazawa's hypothesis that terrestrial Xe fractionation was caused by gravitational separation of adsorbed solar nebular gases inside large porous planetesimals.
K, Zahnle, J B, Pollack, J F, Kasting
openaire   +2 more sources

PLANETESIMALS HERE. PLANETESIMALS THERE. PLANETESIMALS EVERYWHERE

Geological Society of America Abstracts with Programs, 2020
Myriam Telus   +2 more
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Planetesimal rings as the cause of the Solar System’s planetary architecture

Nature Astronomy, 2021
Andre Izidoro   +2 more
exaly  

Sulfur isotopic signature of Earth established by planetesimal volatile evaporation

Nature Geoscience, 2021
Wenzhong Wang   +2 more
exaly  

Linking asteroids and meteorites to the primordial planetesimal population

Geochimica Et Cosmochimica Acta, 2020
Richard C Greenwood, Thomas Burbine
exaly  

Images of Asteroid 21 Lutetia: A Remnant Planetesimal from the Early Solar System

Science, 2011
Hans Rickman   +2 more
exaly  

Planetesimal Population Synthesis: are Planetesimals formed in Pressure Bumps?

2019
Planetesimals, the smallest building blocks of planets that are gravitationally bound, are believed to be needed in order to form planets. The spacial distribution of these objects that are typically 100 km in diameter is important for the outcome of planet formation.
openaire   +1 more source

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