Idade da Terra (Portuguese Wikipedia)

Analysis of information sources in references of the Wikipedia article "Idade da Terra" in Portuguese language version.

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books.google.com

  • Boltwood, B. B. (1907). «On the ultimate disintegration products of the radio-active elements. Part II. The disintegration products of uranium». American Journal of Science. 23: 77–88 
    Para o resumo, veja: Chemical Abstracts Service, American Chemical Society (1907). Chemical Abstracts. New York, London: American Chemical Society. 817 páginas. Consultado em 19 de dezembro de 2008 

doi.org

dx.doi.org

  • Dalrymple, G. Brent (2001). «The age of the Earth in the twentieth century: a problem (mostly) solved». Special Publications, Geological Society of London. 190: 205–221. doi:10.1144/GSL.SP.2001.190.01.14 
  • Manhesa, Gérard; Allègrea, Claude J.; Dupréa, Bernard; and Hamelin, Bruno (1980). «Lead isotope study of basic-ultrabasic layered complexes: Speculations about the age of the earth and primitive mantle characteristics». Earth and Planetary Science Letters, Elsevier B.V. 47: 370–382. doi:10.1016/0012-821X(80)90024-2 
  • Wilde, S. A.; Valley, J. W.; Peck, W. H.; Graham C. M. (11 de janeiro de 2001). «Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago». Nature. 409 (6817): 175–178. PMID 11196637. doi:10.1038/35051550 
  • Wyche, S.; Nelson, D. R.; Riganti, A. (2004). «4350–3130 Ma detrital zircons in the Southern Cross Granite–Greenstone Terrane, Western Australia: implications for the early evolution of the Yilgarn Craton». Australian Journal of Earth Sciences. 51 (1): 31–45. doi:10.1046/j.1400-0952.2003.01042.x 
  • Amelin, Y; Krot, An; Hutcheon, Id; Ulyanov, Aa (2002). «Lead isotopic ages of chondrules and calcium-aluminum-rich inclusions.». Science (New York, N.Y.). 297 (5587): 1678–83. ISSN 0036-8075. PMID 12215641. doi:10.1126/science.1073950 
  • Baker, J.; Bizzarro, M.; Wittig, N.; Connelly, J.; Haack, H. (25 de agosto de 2005). «Early planetesimal melting from an age of 4.5662 Gyr for differentiated meteorites». Nature. 436 (7054): 1127–1131. PMID 16121173. doi:10.1038/nature03882 

nih.gov

ncbi.nlm.nih.gov

  • Wilde, S. A.; Valley, J. W.; Peck, W. H.; Graham C. M. (11 de janeiro de 2001). «Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago». Nature. 409 (6817): 175–178. PMID 11196637. doi:10.1038/35051550 
  • Amelin, Y; Krot, An; Hutcheon, Id; Ulyanov, Aa (2002). «Lead isotopic ages of chondrules and calcium-aluminum-rich inclusions.». Science (New York, N.Y.). 297 (5587): 1678–83. ISSN 0036-8075. PMID 12215641. doi:10.1126/science.1073950 
  • Baker, J.; Bizzarro, M.; Wittig, N.; Connelly, J.; Haack, H. (25 de agosto de 2005). «Early planetesimal melting from an age of 4.5662 Gyr for differentiated meteorites». Nature. 436 (7054): 1127–1131. PMID 16121173. doi:10.1038/nature03882 

usgs.gov

pubs.usgs.gov

wisc.edu

geology.wisc.edu

  • Valley, John W.; Peck, William H.; Kin, Elizabeth M. (1999). «Zircons Are Forever» (PDF). The Outcrop, Geology Alumni Newsletter. University of Wisconsin-Madison. pp. 34–35. Consultado em 22 de dezembro de 2008 

worldcat.org

  • Amelin, Y; Krot, An; Hutcheon, Id; Ulyanov, Aa (2002). «Lead isotopic ages of chondrules and calcium-aluminum-rich inclusions.». Science (New York, N.Y.). 297 (5587): 1678–83. ISSN 0036-8075. PMID 12215641. doi:10.1126/science.1073950