Cinturó supracortical d'Isua: diferència entre les revisions

 

== Bibliografia ==

* Appel, Peter W.U., Hugh R. Rollinson, y Jacques L.R. Touret. (2001) "Remnants of an Early Archaean (>3.75 Ga) sea-floor, hydrothermal system in the Isua Greenstone Belt." ''Precambrian Research'', Vol. 112, números 1-2, 15 de novembre, pp. 27-49.

* Appel, Peter W.U.; C.M Fedo; J.S. Myers. (2001a) "Depositional setting and paleogeographic implications of Earth's oldest supracrustal rocks, the > 3.7 Ga Isua Greenstone belt, West Greenland." ''Sedimentary Geology'', Vol.141, pp. 61-77. Sumari online: {{ref-web|url=http://serials.cib.unibo.it/cgi-ser/start/it/spogli/df-s.tcl?prog_art=4047117&language=ITALIANO&view=articoli|títol=Enllaç<!--Títol generat per bot-->}}

* Rapp, Robert P. (1999) "First Origins of Archean Continental Crust: Assessing Experimentally the Roles of Mafic Versus Ultramafic Sources." Dept. of Geosciences, State University of New York.{{ref-web|url=http://www.the-conference.com/JConfAbs/4/140.html|títol=Enllaç<!--Títol generat per bot-->}}

* Rollinson, Hugh. (1999) "TTG Genesis and Archaean Crustal Growth." Journal of Conference Abstracts, Vol. 4: No. 1, Symposium A08. Early Evolution of the Continental Crust. Online: {{ref-web|url=http://www.the-conference.com/JConfAbs/4/140.html|títol=Enllaç<!--Títol generat per bot-->}}

 

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[[Categoria:Geologia]]

[[Categoria:Geografia de Groenlàndia]]