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Browsing by Author "Pendón Martín, José Gabriel"
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Los foraminíferos bentónicos del horizonte glauconítico inferior de la Formación «Arcillas de Gibraleón» (Depresión del Guadalquivir, SO España)
González-Regalado Montero, María Luz
; Ruiz Muñoz, Francisco; Abad de los Santos, Manuel; Pendón Martín, José Gabriel; Tosquella Angrill, Josep (Sociedad Geológica de España, 2005)
This paper analyzes the benthic foraminiferal assemblages present in two Upper Tortonian sections belonging to the «Arcillas de Gibraleón» Formation (Guadalquivir Basin) containing a characteristic glauconitic level. The ... -
Los ostrácodos del horizonte glauconítico inferior de la Formación “Arcillas de Gibraleón” (Depresión del Guadalquivir, SO España)
Ruiz Muñoz, Francisco; Abad de los Santos, Manuel; Pendón Martín, José Gabriel; González-Regalado Montero, María Luz; Rosa Díaz, Jesús de la; Tosquella Angrill, Josep (Sociedad Geológica de España, 2004)
The analysis of the ostracod assemblages collected in the lower glauconitic horizon of the Arcillas de Gibraleon Formation permits to delimitate two levels: a) Basal level, with the presence of infralittoral, outer ... -
Los ostrácodos infralitorales y circalitorales actuales del norte del Golfo de Cádiz
Ruiz Muñoz, Francisco; González-Regalado Montero, María Luz; Baceta, Juan Ignacio; Pendón Martín, José Gabriel; Hernández Molina, F. Javier; Somoza, L.; Díaz del Río, Víctor (Sociedad Geológica de España, 1999)
The study of the ostracod distribution in the inner part of the Spanish continental she/fallows to recognize the presence of a zonation which reflects changes in both depth and substrate. Four assemblages may be distinguished: ... -
Ostrácodos Tortonienses del Sector Central de la Cuenca del Guadalquivir (Sur de España)
Ruiz Muñoz, Francisco; Abad de los Santos, Manuel; Pendón Martín, José Gabriel; González-Regalado Montero, María Luz; Tosquella Angrill, Josep (Sociedad Geológica de España, 2003)
This paper analyzes the lithostratigraphic features and the ostracode assemblages of the Upper Tortonian deposits located in the central sector of the Guadalquivir basin. Seven facies were defined, being deposited in fluvial ... -
Paleoecología de los niveles lumaquélicos con Heterostegina en el Tortoniense del sector central de la Cuenca del Guadalquivir (SO España)
Tosquella Angrill, Josep; Abad de los Santos, Manuel; González-Regalado Montero, María Luz; Ruiz Muñoz, Francisco; Pendón Martín, José Gabriel (Sociedad Geológica de España, 2002)
The Iumaquellic levels with Heterostegina in a detritic-bioclastic succession (Km 98 section) located in the central sector of the Guadalquivir Basin has been studied. The sedimentological and micropaleontological analysis ... -
Respuesta Estratigráfica a la Transgresión Tortoniense en el Margen Pasivo de la Cuenca del Guadalquivir: Datos Preliminares
Abad de los Santos, Manuel; Pendón Martín, José Gabriel; Ruiz Muñoz, Francisco; Rodríguez Vidal, Joaquín; López González, Nieves; Mantero, Isabel (Sociedad Geológica de España, 2005)
The passive margin of the Guadalquivir foreland basin records different stages of evolution during the tortonian transgression, mainly determinate by sedimentary supply/ accommodation space ratio (A/S ratio, Cattaneo and ... -
Submedios asociados a un sector intermareal de la ría de Huelva
Borrego Flores, José; Morales González, Juan Antonio; Pendón Martín, José Gabriel (Sociedad Geológica de España, 1989)
Varios sedimentary subenvironments relationed to the Huelva Ria are described. In this way there are identified the active channel-margin, the salt-marsh and the sterilemarsh environments. The sequenial arangement is of ... -
Transgressive sequences on foreland margins : a cause studie of the neogene central Guadalquivir basin, southern Spain
Pendón Martín, José Gabriel; Ruiz Muñoz, Francisco; Abad de los Santos, Manuel; González-Regalado Montero, María Luz; Baceta, Juan Ignacio; Tosquella Angrill, Josep (Università degli Studi di Milano, 2004-07)
The Guadalquivir foreland basin, located between the Iberian basement northward and the Betic orogen to the South, repre¬sents the western sector of the earlier foredeep basin of the Betic Cor¬dillera. Along the northern ...
