Thesis Collection
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Browsing by Author "Polo, María Dolores"
Now showing items 1-6 of 6
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Cambios eustáticos y arquitectura estratigráfica de unidades costeras
(Sociedad Geológica de España, 1996)Eustatic movements generate intricate patterns of coastal units. The resulting stratigraphyc architecture depends on eustasy, sediment supply and local tectonics. Tri-dimensional relations due to sea-level changes are ... -
Cyclic coastal sedimentation in Sorbas (Messinian, SE Spain)
(2013)Shifts of the shoreline in the Late Messinian Sorbas Member can be correlated with oscillations of the precession index and eccentricity curves. Close inspection reveals three orders of sea level oscillations with variable ... -
Dunas eólicas y facies asociadas pleistocenas y holocenas en el acantilado del Asperillo (Huelva)
Dabrio, Cristino José; Borja Barrera, Francisco
; Zazo, C.; Boersma, J. R.; Lario, J.; Goy, José L.; Polo, María Dolores (Sociedad Geológica de España, 1996)
Facies analysis and tridimensional relationships of the eolian and eolian-connected deposits of Pleistocene and Holocene age in Huelva allow to propose sedimentary models and discuss their temporal evolution and chronology -
Late Messinian coastal barrier and washover fan sedimentation in Sorbas (SE Spain)
(Sociedad Geológica de España, 1996)Deposition of washo ver fans in coastal settings are related to accommodation space, slope of the basin margin, and coeval changes of sea level. Some preliminary models of development and stacking of sand bodies are presented -
Modelos arrecifales neógenos de la depresión del río Almanzora (Almería)
(Sociedad Geológica de España, 1986)Two models of reef growth are proposed for the Neogene reefs interbedded into the siliciclastic rocks of the narrow, fault-controlled Almanzora Basin: patch reefs on activelyprograding fan deltas (e.g. Purchena and Serón) ... -
Oscilaciones eustáticas de alta frecuencia en el Neógeno superior de Sorbas (Almería, sureste de España)
(Sociedad Geológica de España, 1995)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 ...
