Three-dimensional geometry and interference of fault-bend folds: examples from the Ponga Unit, Variscan Belt, NW Spain

Author:

Alvarez-Marron J.

Publisher

Elsevier BV

Subject

Geology

Reference40 articles.

1. La estructura del sector meridional de las unidades del Aramoy Cuenca Carbonífera Central;Aller,1986

2. Sequences of thrusts and displacement transfer in the superposed duplexes of the Esla Nappe Region (Cantabrian Zone, NW Spain);Alonso;J. Struct. Geol.,1987

3. Alonso J.L., Pulgar J.A., Garcia-Ramos J.C. & Barba P. In press. Tertiary basins and alpine tectonics in the Cantabrian Mountains (NW Spain). In: Tertiary Basins of Spain. Tectonics, Climate and Sea-Level Changes (edited by Friend P.F. & Dadriao, C). Cambridge University Press.

4. Kinematic models of deformation at an oblique ramp;Apotria,1992

5. La estructura geológica de la Región del Ponga (Zona Cantábrica, NW de Espana). Servicio de Publicaciones de Tesis Doctorales;Alvarez-Marron,1989

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