Buscar
Mostrando ítems 1-10 de 38
Flexural isostasy in the Bolivian Andes: Chaco foreland basin development
(Elsevier Science, 2009-09)
The Chaco foreland basin was initiated during the late Oligocene as a result of thrusting in the Eastern Cordillera in response to Nazca-South America plate convergence. Foreland basins are the result of the flexural ...
Um Breve Histórico de Conceitos Fundamentais da Estratigrafia Moderna: Sequências Deposicionais e seus Fatores Controladores
(Instituto de Geociências /Universidade Federal do Rio Grande do Sul, 1998)
Thermal and geodynamic contributions to the elevation of the Altiplano-Puna plateau
(Elsevier Science, 2014-10)
The most remarkable feature of the Central Andes is the Altiplano–Puna plateau. This plateau is characterized by 3.5 km average elevation, approximately 70 km crustal thickness and very high heat flow. The upper mantle ...
Study of the Claromecó Basin from gravity, magnetic and geoid undulation charts
(Instituto de Fisiografía y Geología. Facultad de Ciencias Exactas, Ingeniería y Agrimensura. Universidad Nacional de Rosario, 2012)
LIFFE: Lithospheric flexure with finite elements
(Pergamon-Elsevier Science Ltd, 2020-07)
We present LIFFE (Lithospheric Flexure with Finite Elements), a platform designed to perform lithospheric flexure. LIFFE is an easy-to-use, flexible and open-source code intended to model the flexure of a laterally ...
Alternative gravimetric methodology for isostatic analyses. An example for Bolivian Andes
(Instituto de Fisiografía y Geología, 2009)