@article{10272/18093,
year = {1990},
url = {http://hdl.handle.net/10272/18093},
abstract = {The presence of clorithic nodules inside low grade metamorphic rocks (Purbeck-Weald facies), to the NE of Agreda (Soria), has allowed to characterize, by means of the Rf/Ø technique, an oblate strain ellipsoid with k=0.70. The moderate rate of shortening that this type of ellipsoid implies has a close relationship with the macroestructural features},
abstract = {La presencia de nódulos cloríticos dentro del bajo ángulo metamórfico de las rocas (facies Purbeck-Weald), al NE de Agreda (Soria), nos ha permitido describir, por medio de la técnica Rf/Ø, un elipsoide de deformación achatada con k=0,70. La tasa intermedia de acortamiento que implica este tipo de elipsoide tiene una relación estrecha con las características macroestructurales.},
publisher = {Sociedad Geológica de España},
keywords = {Clorithic nodules},
keywords = {Oblate strain ellipsoid},
title = {Aplicación del método Rf/ø al análisis de la deformación finita de los materiales wealdenses de Agreda (Soria)},
title = {Application of Rf/ø method to the finite strain analysis of the wealdian deposits ofAgreda (Soria)},
author = {Gil Imaz, Andrés and Pocoví Juan, Andrés},
}