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Resultats globals: 3 registres trobats en 0.01 segons.
Articles, 3 registres trobats
Articles 3 registres trobats  
1.
19 p, 2.3 MB The Case for UHP Conditions in the Cuaba Terrane, Río San Juan Metamorphic Complex, Dominican Republic / Abbott, R. N. (Appalachian State University. Department of Geology) ; Draper, G. (Florida International University. Department of Earth Sciences)
From the Cuaba terrane in northern Dominican Republic. Ultrahigh pressure (UHP) conditions are indicated for the Cuaba terrane on the basis of phase relationships in garnet-bearing ultramafic rock. Dikes and orthocumulate textures indicate a magmatic origin. [...]
2013 - 10.1344/105.000001841
Geologica acta, Vol. 11, Núm. 2 (Juny 2013) , p. 149-165  
Registre complet - Creative Commons
2.
39 p, 5.2 MB Foundations of Gulf of Mexico and Caribbean evolution : eight controversies resolved / Pindell, J. (Rice University. Department of Earth Science) ; Kennan, L. (Tectonic Analysis Ltd.) ; Draper, G. (Florida International University. Department of Earth Sciences) ; Maresch, W. V. (Ruhr-Universität Bochum. Institut für Geologie, Mineralogie und Geophysik) ; Stanek, K. P. (TU Bergakademie Freiberg. German Institut für Geologie)
Eight points of recurring controversy regarding the primary foundations of models of Gulf of Mexico and Caribbean tectonic evolution are identified and examined. The eight points are controversial mainly because of the disconnect between different scales of thinking by different workers, a common but unfortunate problem in the geological profession. [...]
2006 - 10.1344/105.000000371
Geologica acta, Vol. 4, Núm. 1-2 (2006) , p. 303-341  
Registre complet - Creative Commons
3.
27 p, 1.3 MB Ophiolite-Related Ultramafic Rocks (Serpentinites) in the Caribbean Region : a Review of their Occurrence, Composition, Origin, Emplacement and Ni-Laterite Soil Formation / Lewis, J. F. (The George Washington University. Department of Earth and Environmental Sciences) ; Draper, G. (Florida International University. Department of Earth Sciences) ; Espaillat, J. (Corporación Minera Dominicana) ; Proenza, J. A. (Universitat de Barcelona. Departament de Cristal·lografia, Mineralogia i Dipòsits Minerals) ; Jiménez, J. (Falconbridge Dominicana)
Ultramafic rocks, mainly serpentinized peridotites of mantle origin, are mostly associated with the ophiolites of Mesozoic age that occur in belts along three of the margins of the Caribbean plate. The most extensive exposures are in Cuba. [...]
2006 - 10.1344/105.000000368
Geologica acta, Vol. 4, Núm. 1-2 (2006) , p. 237-263  
Registre complet - Creative Commons

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