Origen de las piritas de la cuenca de Cameros, (La Rioja)
The pyrite mineralizations of the Cameros basin has been traditionally interpreted as diagenetic. On the basis of trace element content, S isotopes study, pyrite inclusions and geologic observations, the pyrite crystals seem to be associated to a mobilization process of previous sedimentary pyrites...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1995 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/13547 |
| Acceso en línea: | http://hdl.handle.net/10272/13547 |
| Access Level: | acceso abierto |
| Palabra clave: | Pyrite Mobilization Hydrothermal metamorphism |
| Sumario: | The pyrite mineralizations of the Cameros basin has been traditionally interpreted as diagenetic. On the basis of trace element content, S isotopes study, pyrite inclusions and geologic observations, the pyrite crystals seem to be associated to a mobilization process of previous sedimentary pyrites during the hydrothermal metamorphism that affected the basin |
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