Accretion of Phobos and Deimos in an extended debris disc stirred by transient moons View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2016-07-04

AUTHORS

Pascal Rosenblatt, Sébastien Charnoz, Kevin M. Dunseath, Mariko Terao-Dunseath, Antony Trinh, Ryuki Hyodo, Hidenori Genda, Stéven Toupin

ABSTRACT

Mars has two small moons that may have formed in the aftermath of a giant impact. Simulations suggest that Phobos and Deimos accreted from the disperse outer region of the debris disc that was stirred up by short-lived larger moons.

PAGES

581-583

References to SciGraph publications

  • 2011-08-26. The origin of the Martian moons revisited in THE ASTRONOMY AND ASTROPHYSICS REVIEW
  • 1990-03. Symplectic integrators and their application to dynamical astronomy in CELESTIAL MECHANICS AND DYNAMICAL ASTRONOMY
  • 2015-11-23. The demise of Phobos and development of a Martian ring system in NATURE GEOSCIENCE
  • 2010-06. The recent formation of Saturn's moonlets from viscous spreading of the main rings in NATURE
  • 1985. An Efficient Integrator that Uses Gauss-Radau Spacings in DYNAMICS OF COMETS: THEIR ORIGIN AND EVOLUTION
  • Identifiers

    URI

    http://scigraph.springernature.com/pub.10.1038/ngeo2742

    DOI

    http://dx.doi.org/10.1038/ngeo2742

    DIMENSIONS

    https://app.dimensions.ai/details/publication/pub.1038813348


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