Results 181 to 190 of about 3,499 (221)
Carbon and oxygen isotope evidence for a protoplanetary disk origin of organic solids in meteorites. [PDF]
Lawrence WM, Blake GA, Eiler J.
europepmc +1 more source
Formation of Lunar Basins from Impacts of Leftover Planetesimals
Nesvorny D +6 more
europepmc +1 more source
When wet meets dry: An Ivuna-like impactor triggered volatile loss on the angrite parent body. [PDF]
Zhu 朱柯 K +5 more
europepmc +1 more source
Magnesium phosphates experienced high-temperature transition found on the CI-like carbonaceous chondrite Yamato 980115 by Raman microspectroscopy. [PDF]
Yui H +6 more
europepmc +1 more source
Recent progress and future prospects of the early solar system chronology. [PDF]
Amelin Y, Yin QZ.
europepmc +1 more source
Decoding the formation of barred olivine chondrules: Realization of numerical replication. [PDF]
Miura H +6 more
europepmc +1 more source
Processes governing the evolution of planetesimals are critical to understanding how rocky planets are formed, how water is delivered to them, the origin of planetary atmospheres, how cores and magnetic dynamos develop, and ultimately, which planets have the potential to be habitable.
core +3 more sources
Small planetesimals in a massive disk formed Mars
Mars is likely to be a planetary embryo formed through collisions with planetesimals, which can explain its small mass and rapid formation timescale obtained from 182Hf-182W chronometry.
Nicolas Dauphas
exaly +2 more sources
Impact disruption of primordial planetesimals [PDF]
It isusually assumed that 1-10-km sized planetesimals are formed through coagulation processes and continue to agglomerate via pairwise mergers.
Parisi, Mirta Gabriela
exaly +2 more sources

