La utilización de la anisotropía de la susceptibilidad magnética (ASM) en el estudio de la deformación finita: ejemplo en la zona milonítica de Cap de Creus (Catalunya)
The magnetic susceptibility anisotropy (MSA) of the Roses Granodiorite has been studied The magnetic fabric is due to the shear zones that affect these rocks. In this sense, the kmin axes of the MSA are paralel to the foliation poles and the kmax axes are parallel to the direction of the mineral elo...
| Autor: | |
|---|---|
| Formato: | artículo |
| Fecha de publicación: | 1988 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18380 |
| Acesso em linha: | http://hdl.handle.net/10272/18380 |
| Access Level: | acceso abierto |
| Palavra-chave: | Anisotropy of magnetic susceptibility Shear zone Roses Granodiorite |
| Resumo: | The magnetic susceptibility anisotropy (MSA) of the Roses Granodiorite has been studied The magnetic fabric is due to the shear zones that affect these rocks. In this sense, the kmin axes of the MSA are paralel to the foliation poles and the kmax axes are parallel to the direction of the mineral elongation measured in the field The Flinn-type diagram to study the ellipsoid shape indicates oblateness of the MSA ellipsoid |
|---|