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Carbonate systems during the Olicocene-Miocene Climatic Transition.
The Oligocene and Miocene Epochs comprise the most important phases in the Cenozoic global cooling that led from a greenhouse to an icehouse Earth. Recent major advances in the understanding and time-resolution of climate events taking place at this time, as well as the proliferation of studies on O...
| Clasificación: | Libro Electrónico |
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| Autor principal: | |
| Otros Autores: | , |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
Chichester :
John Wiley & Sons,
2010.
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| Temas: | |
| Acceso en línea: | Texto completo |
Tabla de Contenidos:
- Carbonate Systems During the OligoceneMiocene Climatic Transition; Contents; Miocene carbonate systems: an introduction; A synthesis of Late Oligocene through Miocene deep sea temperatures as inferred from foraminiferal Mg/Ca ratios; Latitudinal trends in Cenozoic reef patterns and their relationship to climate; Carbonate grain associations: their use and environmental significance, a brief review.
- Temperate and tropical carbonate-sedimentation episodes in the Neogene Betic basins (southern Spain) linked to climatic oscillations and changes in Atlantic-Mediterranean connections: constraints fromFacies models and geometries of the Ragusa Platform (SE Sicily, Italy) near the SerravallianTortonian boundary; The sensitivity of a tropical foramol-rhodalgal carbonate ramp to relative sea-level change: Miocene of the central Apennines, Italy; Facies and sequence architecture of a tropical foramol-rhodalgal carbonate ramp: Miocene of the central Apennines (Italy).
- Facies and stratigraphic architect.