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International Journal of Geophysics
Volume 2010, Article ID 146496, 16 pages
Research Article

A Magma Accretion Model for the Formation of Oceanic Lithosphere: Implications for Global Heat Loss

1Coordenadoria de Geofísica, Observatório Nacional—MCT, Rua General José Cristino, CEP 20921-400, Rio de Janeiro, Brazil
2Instituto de Ciência e Tecnologia do Mucuri, Universidade Federal dos Vales do Jequitinhonha e Mucuri, CEP 39800-000, Teófilo Otoni, Brazil

Received 28 October 2009; Revised 24 February 2010; Accepted 7 March 2010

Academic Editor: Shuichi Kodaira

Copyright © 2010 Valiya M. Hamza et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Citations to this Article [4 citations]

The following is the list of published articles that have cited the current article.

  • V. M. Hamza, and F. P. Vieira, “Global distribution of the lithosphere-asthenosphere boundary: a new look,” Solid Earth, vol. 3, no. 2, pp. 199–212, 2012. View at Publisher · View at Google Scholar
  • A.M. Hofmeister, and R.E. Criss, “How irreversible heat transport processes drive Earth's interdependent thermal, structural, and chemical evolution,” Gondwana Research, 2013. View at Publisher · View at Google Scholar
  • Roberta A. Cardoso, and Valiya M. Hamza, “Heat Flow in the Campos Sedimentary Basin and Thermal History of the Continental Margin of Southeast Brazil,” ISRN Geophysics, vol. 2014, pp. 1–19, 2014. View at Publisher · View at Google Scholar
  • Jian Wang, Chun-Feng Li, and Yu Lu, “A global reference model of Curie-point depths based on EMAG2,” Scientific Reports, vol. 7, 2017. View at Publisher · View at Google Scholar