Abstract
Previous articleNext article FreeDiastrophism and the Formative Processes XIII. The Bearings of the Size and Rate of Infall of Planetesimals on the Molten or Solid State of the EarthT. C. ChamberlinT. C. Chamberlin Search for more articles by this author PDFPDF PLUS Add to favoritesDownload CitationTrack CitationsPermissionsReprints Share onFacebookTwitterLinkedInRedditEmail SectionsMoreDetailsFiguresReferencesCited by The Journal of Geology Volume 28, Number 8Nov - Dec., 1920 Article DOIhttps://doi.org/10.1086/622742 Views: 26Total views on this site Citations: 4Citations are reported from Crossref PDF download Crossref reports the following articles citing this article:Stephen G. Brush Is the Earth too old? The impact of geochronology on cosmology, 1929–1952, Geological Society, London, Special Publications 190, no.11 (Jan 2001): 157–175.https://doi.org/10.1144/GSL.SP.2001.190.01.12 Verne R. Oberbeck , John R. Marshall , and Hans Aggarwal Impacts, Tillites, and the Breakup of Gondwanaland, The Journal of Geology 101, no.11 (Sep 2015): 1–19.https://doi.org/10.1086/648193Ellis Yochelson, Stephen Brush The Age of the Earth in the Twentieth Century, Earth Sciences History 8, no.22 (Jan 1989): 170–182.https://doi.org/10.17704/eshi.8.2.l555205161r6pvu3Stephen G. Brush A Geologist among Astronomers: The Rise and Fall of the Chamberlin-Moulton Cosmogony, Part 2, Journal for the History of Astronomy 9, no.22 (Jun 1978): 77–104.https://doi.org/10.1177/002182867800900201
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