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Mostrando ítems 1-10 de 2049
THE PERNAMBUCO-ALAGOAS MASSIF, NORTHEAST BRAZILTHE PERNAMBUCO-ALAGOAS MASSIF, NORTHEAST BRAZIL
(Sociedade Brasileira de Geologia, 2018)
THE MASSIFICATION PROCESS IN CHINESE HIGHER EDUCATION
(INPEAU, 2015)
Significance of the early Jurassic Garamilla formation in the Western Nordpatagonian Massif
(Pergamon-elsevier Science Ltd, 2013-03)
By means of facial, stratigraphic, petrographic, geochemical and geochronological studies we characterize the Garamilla Formation, cropping out in the western Nordpatagonian Massif. The studies of these volcanic rocks ...
Blended Learning as the Best Scenario for Institutions Affected by Massification
Massification is a problem affecting universities around the world, given the increase in student enrolments. Teaching in a large classroom containing a huge number of students is a great challenge for teachers. Cadi Ayyad ...
Jurassic hot spring deposits of the Deseado Massif (Patagonia, Argentina): Characteristics and controls on regional distribution
(Elsevier Science, 2011-06)
The Deseado Massif, Santa Cruz Province, Argentinean Patagonia, hosts numerous Middle to Late Jurassic age geothermal and epithermal features represented by siliceous and calcareous chemical precipitates from hot springs ...
Paleo-landscapes of the Northern Patagonian Massif, Argentina
(Springer, 2014)
The dominant geomorphological unit of the Northern Patagonian Massif landscape is a regional planation surface, eroded across the crystalline basement, and eruptive rocks of the Gondwana cycle, and Jurassic volcanic rocks. ...
Mapping glacial landforms on the Chirripó massif, Costa Rica, based on Google Earth, a digital elevation model, and field observations.
(Universidad de Costa Rica, 2019)
Structure and U-Pb dating of the Saint-Arnac pluton and the Ansignan charnockite (Agly Massif): a cross-section from the upper to the middle crust of the Variscan Eastern Pyrenees
(GEOLOGICAL SOC PUBL HOUSE, 2008-01)
In the Agly Massif (Pyrenees), two Variscan plutons, the Saint-Arnac pluton and the Ansignan
charnockite, intrude different levels of a c. 10 km thick crustal section. The Saint-Arnac pluton intrudes
through upper crustal ...