Cinturó supracortical d'Isua: diferència entre les revisions
Contingut suprimit Contingut afegit
Línia 13:
==Bibliografia==
<small>
* 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
* Appel, Peter W.U.
* Bickle, Michael James
* Dann, J.C., T.L. Grove, y S.W. Parman. (2001) "The production of Barberton komatiites in an Archean subduction zone." ''Geophysical Research Letters'',
* Frei, Robert y Minik T. Rosing. (1999) "Late Archaean Metasomatism and Kyanite Formation in the >3700 Ma Isua Supracrustals, West Greenland."
* Myers, John S. (2001) "Protoliths of the 3.8-3.7 Ga Isua greenstone belt, West Greenland." ''Precambrian Research'',
* Myers, John. (1999) "Protoliths of the c. 3.7 Ga Isua Greenstone Belt, West Greenland." ''Journal of Conference Abstracts'', Vol. 4,
* Polat, A., Hofmann, A.W., y Rosing, M.T., 2002. Boninite-like volcanic rocks in the 3.7-3.8 Ga Isua greenstone belt, West Greenland: geochemical evidence for intra-oceanic subduction zone processes in the early Earth. Chemical Geology, '''184''': 231-254.
* 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.[http://www.the-conference.com/JConfAbs/4/140.html]
| |||