Oscilaciones eustáticas de alta frecuencia en el Neógeno superior de Sorbas (Almería, sureste de España)
A brief description of detail stratigraphy of the Late-Neogene Terminal Carbonate Complex and the Sorbas Member, and the precise role of the stromatolite layers that occur interbedded. The vicinity to the sources of coarse-gained sediment input, mobility of the sea-bottom, and the topographic elevat...
| 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:10272/13548 |
| Acceso en línea: | http://hdl.handle.net/10272/13548 |
| Access Level: | acceso abierto |
| Palabra clave: | Mixed shelf Fringing reefs Stromatolites Talus slope Eustatic oscillations Late Neogene South-eastern Spain |
| Sumario: | A brief description of detail stratigraphy of the Late-Neogene Terminal Carbonate Complex and the Sorbas Member, and the precise role of the stromatolite layers that occur interbedded. The vicinity to the sources of coarse-gained sediment input, mobility of the sea-bottom, and the topographic elevation reached by the sea during high stands of4th/5th order oscillations control the development of stromatolites. Recognition of high-frequency (fourth and fifth-order cycles) inside a third-order (TB 3.4)'eustatic cycle |
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