Add to ORKG[EN]The Guadalquivir Basin si an important depression, elongated in the ENE-WSW direction, which is almost enterly made up of soft sediments. Starting at the eastern end it has an altitude of more tgan 800 m. above sea level, descending gradually to the west, reaching the coast, in the provinces of Huelva and Cádiz. Sedimentation continues today below sea leven in the Gulf of Cádiz
The Guadalquivir foreland basin, located between the Iberian basement northward and the Betic orogen...
In this study the development and recent evolution of the drainge within the Guadalentín Depression ...
The Neogene succession of the eastern part of the Guadalquivir basin was found to consist from bott...
A detailed surveying and a new geological map of the sheet at 1:50.000 number 999/1016 (Huelva - Los...
In the Neogene sediments of the western part of the Guadalquivir Basin eight formations have been d...
A multidisciplinary analysis of cores and geomorphic patterns in the marshes of Doñana National Park...
Thè marine arid lacustrine Upper Neogene sediments in the Southwestern sector of the Guadalquivir Ba...
The paleontological data of the marine neogene sediments in the Lepe-Ayamonte area, Huelva (SW of th...
Las diferentes formaciones (Tortoniense-Plioceno inferior), que se han distinguido en la cuenca del ...
Spain) has yielded new evidence regarding the sedimentary infilling and geomorphological evolution o...
The sedimentary environment of the Guadix-Baza Depression sediments, between Upper Miocene and Upper...
5th International Geologica Belgica Meeting, 26-29 January 2016, Mons, BelgiumWe have investigated t...
The Empordci basin is located at the northeast of the Iberian Peninsula in this Basin several deltai...
The Guadix topographic depression is a Neogene-Quaternary basin located in the central sector of the...
NW-SE oriented intramontane depression, filled by an up to 1,200 m- thick succession of lacustrine a...
The Guadalquivir foreland basin, located between the Iberian basement northward and the Betic orogen...
In this study the development and recent evolution of the drainge within the Guadalentín Depression ...
The Neogene succession of the eastern part of the Guadalquivir basin was found to consist from bott...
A detailed surveying and a new geological map of the sheet at 1:50.000 number 999/1016 (Huelva - Los...
In the Neogene sediments of the western part of the Guadalquivir Basin eight formations have been d...
A multidisciplinary analysis of cores and geomorphic patterns in the marshes of Doñana National Park...
Thè marine arid lacustrine Upper Neogene sediments in the Southwestern sector of the Guadalquivir Ba...
The paleontological data of the marine neogene sediments in the Lepe-Ayamonte area, Huelva (SW of th...
Las diferentes formaciones (Tortoniense-Plioceno inferior), que se han distinguido en la cuenca del ...
Spain) has yielded new evidence regarding the sedimentary infilling and geomorphological evolution o...
The sedimentary environment of the Guadix-Baza Depression sediments, between Upper Miocene and Upper...
5th International Geologica Belgica Meeting, 26-29 January 2016, Mons, BelgiumWe have investigated t...
The Empordci basin is located at the northeast of the Iberian Peninsula in this Basin several deltai...
The Guadix topographic depression is a Neogene-Quaternary basin located in the central sector of the...
NW-SE oriented intramontane depression, filled by an up to 1,200 m- thick succession of lacustrine a...
The Guadalquivir foreland basin, located between the Iberian basement northward and the Betic orogen...
In this study the development and recent evolution of the drainge within the Guadalentín Depression ...
The Neogene succession of the eastern part of the Guadalquivir basin was found to consist from bott...