dc.creatorGuilera, Octavio Miguel
dc.creatorSwoboda, D.
dc.creatorAlibert, Y.
dc.creatorElía, Gonzalo Carlos de
dc.creatorSantamaría, Pablo Javier
dc.creatorBrunini, Adrián
dc.date2014
dc.date2019-11-11T13:41:08Z
dc.identifierhttp://sedici.unlp.edu.ar/handle/10915/85287
dc.identifierissn:1743-9213
dc.descriptionIn the standard model of core accretion, the cores of the giant planets form by the accretion of planetesimals. In this scenario, the evolution of the planetesimal population plays an important role in the formation of massive cores. Recently, we studied the role of planetesimal fragmentation in the in situ formation of a giant planet. However, the exchange of angular momentum between the planet and the gaseous disk causes the migration of the planet in the disk. In this new work, we incorporate the migration of the planet and study the role of planet migration in the formation of a massive core when the population of planetesimals evolves by planet accretion, migration, and fragmentation.
dc.descriptionInstituto de Astrofísica de La Plata
dc.descriptionFacultad de Ciencias Astronómicas y Geofísicas
dc.formatapplication/pdf
dc.format204-207
dc.languageen
dc.rightshttp://creativecommons.org/licenses/by-nc-sa/4.0/
dc.rightsCreative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
dc.subjectCiencias Astronómicas
dc.subjectplanet migration
dc.subjectplanetary systems: formation
dc.subjectplanetesimal fragmentation
dc.titlePlanetesimal fragmentation and giant planet formation: the role of planet migration
dc.typeArticulo
dc.typeComunicacion


Este ítem pertenece a la siguiente institución