Hydrothermal alteration of magnetic fabrics of rocks in the Xiaoban gold-bearing shear belt, Fujian Province, China

Magnetic fabrics indicate that the Xiaoban shear zone underwent low-grade hydrothermal alteration in the Mesozoic (180Ma). Samples studied come from altered and unaltered units from three mine levels. (1) Susceptibility is mainly due to paramagnetic minerals such as biotite and pyrite. The reduction...

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Detalles Bibliográficos
Autores: Wu, Ganguo, Wu, Jianshe, Chen, Bailin
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2003
País:México
Institución:UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO
Repositorio:Geofísica Internacional
Idioma:español
OAI Identifier:oai:revistagi.geofisica.unam.mx:article/874
Acceso en línea:http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/874
Access Level:acceso abierto
Palabra clave:Fábrica magnética
susceptibilidad
anisotropía
alteración hidrotermal
China
Magnetic fabric
susceptibility
anisotropy
hydrothermal alteration
Descripción
Sumario:Magnetic fabrics indicate that the Xiaoban shear zone underwent low-grade hydrothermal alteration in the Mesozoic (180Ma). Samples studied come from altered and unaltered units from three mine levels. (1) Susceptibility is mainly due to paramagnetic minerals such as biotite and pyrite. The reduction of mean susceptibility is due to decrease in Fe content and change of magnetic mineral size, as well as increase of diamagnetic minerals. (2) Anisotropy (P) decreases after hydrothermal alteration. Its tendency to change is the same as that of the mean susceptibility. (3) The AMS ellipsoid does not substantially change its shape after hydrothermal alteration. An oblate sphere is maintained. The minimum principal susceptibility axis (K3) falls close to the plane which is perpendicular to the schistosity for all samples. However, the maximum principal susceptibility axis is subject to large changes. The results indicate that new magnetic minerals are distributed on the existing schistosity plane, without a preferred orientation.