Arrecifes Messinienses de Almería. Tipologías de crecimiento, posición estratigráfica y relación con las evaporitas
Messinian reefs in the Almería area developed mainly as pinnacle and fringing reefs. Both types of reefs grade laterally, basinwards, to yellowish, silty marls and diatomites and clearly underlie the Messinian gypsum deposited in the centre of the basins
| Authors: | ; |
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| Format: | Article |
| Publication date: | 1989 |
| Country: | España |
| Institution: | Universidad de Huelva (UHU) |
| Repository: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Language: | Spanish |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18207 |
| Online Access: | http://hdl.handle.net/10272/18207 |
| Access Level: | Open access |
| Keyword: | Messinian stratigraphy Reefs and evaporites Diatomites |
| Summary: | Messinian reefs in the Almería area developed mainly as pinnacle and fringing reefs. Both types of reefs grade laterally, basinwards, to yellowish, silty marls and diatomites and clearly underlie the Messinian gypsum deposited in the centre of the basins |
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