Diapiro de Salinas de Añana: ¿un diapiro con un Overhang? Modelo 3D grav¡mético

V. Pinto; A. Casas; X. Font

doi:10.3989/egeol.98543-4211

Diapiro de Salinas de Añana: ¿un diapiro con un Overhang? Modelo 3D grav¡mético

Authors

V. Pinto Departamento Geoquímicas, Petrología y Prospección Geológica. Facultad de Geología. Universidad de Barcelona
A. Casas Departamento Geoquímicas, Petrología y Prospección Geológica. Facultad de Geología. Universidad de Barcelona
X. Font Departamento Geoquímicas, Petrología y Prospección Geológica. Facultad de Geología. Universidad de Barcelona

DOI:

https://doi.org/10.3989/egeol.98543-4211

Keywords:

Diapir, 3D model, gravimetry

Abstract

A new gravity map of the Cubeta Alavesa has been compliled and interpreted. In this map the gravity lows produced by the outcropping evaporitic diapirs and other deeper structures are very well depicted. The gravity low of the Salinas de Añana diapir has been modelled using two different 3D methods. The density model obtained has a great extension at surface but not in depth, given a lateral extension or overghang dipping to the SW.

Downloads

Download data is not yet available.

Downloads

Published

1998-08-30

How to Cite

Pinto, V., Casas, A., & Font, X. (1998). Diapiro de Salinas de Añana: ¿un diapiro con un Overhang? Modelo 3D grav¡mético. Estudios Geológicos, 54(3-4), 123–128. https://doi.org/10.3989/egeol.98543-4211

Download Citation

Issue

Vol. 54 No. 3-4 (1998)

Section

Articles

License

This work is licensed under a Creative Commons Attribution 4.0 International License.

© CSIC. Manuscripts published in both the print and online versions of this journal are the property of the Consejo Superior de Investigaciones Científicas, and quoting this source is a requirement for any partial or full reproduction.

All contents of this electronic edition, except where otherwise noted, are distributed under a Creative Commons Attribution 4.0 International (CC BY 4.0) licence. You may read the basic information and the legal text of the licence. The indication of the CC BY 4.0 licence must be expressly stated in this way when necessary.

Self-archiving in repositories, personal webpages or similar, of any version other than the final version of the work produced by the publisher, is not allowed.