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dc.contributor.authorHoward, Andrew W.
dc.contributor.authorMarcy, Geoffrey W.
dc.contributor.authorJohnson, John Asher
dc.contributor.authorIsaacson, Howard
dc.contributor.authorFischer, Debra A.
dc.contributor.authorFulton, Benjamin J.
dc.contributor.authorSinukoff, Evan
dc.contributor.authorFortney, Jonathan J.
dc.contributor.authorSanchis Ojeda, Roberto
dc.contributor.authorWinn, Joshua Nathan
dc.date.accessioned2014-08-11T19:18:49Z
dc.date.available2014-08-11T19:18:49Z
dc.date.issued2013-10
dc.date.submitted2013-09
dc.identifier.issn0028-0836
dc.identifier.issn1476-4687
dc.identifier.urihttp://hdl.handle.net/1721.1/88682
dc.description.abstractPlanets with sizes between that of Earth (with radius R[subscript circle in cross]) and Neptune (about 4 R[subscript circle in cross]) are now known to be common around Sun-like stars. Most such planets have been discovered through the transit technique, by which the planet’s size can be determined from the fraction of starlight blocked by the planet as it passes in front of its star. Measuring the planet’s mass—and hence its density, which is a clue to its composition—is more difficult. Planets of size 2–4 R[subscript circle in cross] have proved to have a wide range of densities, implying a diversity of compositions, but these measurements did not extend to planets as small as Earth. Here we report Doppler spectroscopic measurements of the mass of the Earth-sized planet Kepler-78b, which orbits its host star every 8.5 hours (ref. 6). Given a radius of 1.20 ± 0.09 R[subscript circle in cross] and a mass of 1.69 ± 0.41 M[subscript circle in cross], the planet’s mean density of 5.3 ± 1.8 g cm[superscript −3] is similar to Earth’s, suggesting a composition of rock and iron.en_US
dc.description.sponsorshipKepler Participating Scientist Programen_US
dc.language.isoen_US
dc.publisherNature Publishing Groupen_US
dc.relation.isversionofhttp://dx.doi.org/10.1038/nature12767en_US
dc.rightsCreative Commons Attribution-Noncommercial-Share Alikeen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/en_US
dc.sourcearXiven_US
dc.titleA rocky composition for an Earth-sized exoplaneten_US
dc.typeArticleen_US
dc.identifier.citationHoward, Andrew W., Roberto Sanchis-Ojeda, Geoffrey W. Marcy, John Asher Johnson, Joshua N. Winn, Howard Isaacson, Debra A. Fischer, Benjamin J. Fulton, Evan Sinukoff, and Jonathan J. Fortney. “A Rocky Composition for an Earth-Sized Exoplanet.” Nature 503, no. 7476 (October 30, 2013): 381–384.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Physicsen_US
dc.contributor.departmentMIT Kavli Institute for Astrophysics and Space Researchen_US
dc.contributor.mitauthorSanchis Ojeda, Robertoen_US
dc.contributor.mitauthorWinn, Joshua Nathanen_US
dc.relation.journalNatureen_US
dc.eprint.versionAuthor's final manuscripten_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dspace.orderedauthorsHoward, Andrew W.; Sanchis-Ojeda, Roberto; Marcy, Geoffrey W.; Johnson, John Asher; Winn, Joshua N.; Isaacson, Howard; Fischer, Debra A.; Fulton, Benjamin J.; Sinukoff, Evan; Fortney, Jonathan J.en_US
dc.identifier.orcidhttps://orcid.org/0000-0002-4265-047X
mit.licenseOPEN_ACCESS_POLICYen_US
mit.metadata.statusComplete


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