Add to ORKGThè marine arid lacustrine Upper Neogene sediments in the Southwestern sector of the Guadalquivir Basin (Lepe-Ayamonte area, Huelva, Spain), are basically characterized by four distinte ichnofacies: Cruziana, Skolithos, mixed Cruziana-Skolithos, Gnathichnus and GlóssifungiièS ichrìófacies. The stages of ichnofacial evolution provides several palaeòenviromentàl keys for these materials, as bathimetry, hydrodihamic energy, salinity and type of substratu
A detailed analysis of the Upper Messinian-Lower Pliocene at the northern border of the Bajo Segura ...
En este trabajo se describen los primeros datos sobre los Osteictios de la Formación “Arcillas de Gi...
Hyperpycnal flows have been widely described in different lacustrine and marine environments but sed...
FOREWORD The marine Neogene is well represented in Catalonia and it has been well known and studied ...
An ichnological assemblage from the Upper Miocene bioclastic calcarenites in the Southern edge of th...
The paleontological data of the marine neogene sediments in the Lepe-Ayamonte area, Huelva (SW of th...
[EN]The Guadalquivir Basin si an important depression, elongated in the ENE-WSW direction, which is ...
In the Neogene sediments of the western part of the Guadalquivir Basin eight formations have been d...
An ichnological study was carried out in the Middle–Upper Eocene sedimentary succession of the Pampl...
The Tertiary-age Almazán Basin is located in the western part of the Iberian Range, and formed durin...
A detailed surveying and a new geological map of the sheet at 1:50.000 number 999/1016 (Huelva - Los...
The postglacial interval of the Upper Carboniferous Hoyada Verde Formation of western Argentina cont...
International Ocean Discovery Program Expedition 339 took place in the Gulf of Cadiz and the Western...
The taphonomic analysis of the Osteichthyes and Condrichthyes of the Arenas de Huelva Formation perm...
The Arcas del Villar gypsum sequence (Tagus Basin, Central Spain), previously thought to be Eocene o...
A detailed analysis of the Upper Messinian-Lower Pliocene at the northern border of the Bajo Segura ...
En este trabajo se describen los primeros datos sobre los Osteictios de la Formación “Arcillas de Gi...
Hyperpycnal flows have been widely described in different lacustrine and marine environments but sed...
FOREWORD The marine Neogene is well represented in Catalonia and it has been well known and studied ...
An ichnological assemblage from the Upper Miocene bioclastic calcarenites in the Southern edge of th...
The paleontological data of the marine neogene sediments in the Lepe-Ayamonte area, Huelva (SW of th...
[EN]The Guadalquivir Basin si an important depression, elongated in the ENE-WSW direction, which is ...
In the Neogene sediments of the western part of the Guadalquivir Basin eight formations have been d...
An ichnological study was carried out in the Middle–Upper Eocene sedimentary succession of the Pampl...
The Tertiary-age Almazán Basin is located in the western part of the Iberian Range, and formed durin...
A detailed surveying and a new geological map of the sheet at 1:50.000 number 999/1016 (Huelva - Los...
The postglacial interval of the Upper Carboniferous Hoyada Verde Formation of western Argentina cont...
International Ocean Discovery Program Expedition 339 took place in the Gulf of Cadiz and the Western...
The taphonomic analysis of the Osteichthyes and Condrichthyes of the Arenas de Huelva Formation perm...
The Arcas del Villar gypsum sequence (Tagus Basin, Central Spain), previously thought to be Eocene o...
A detailed analysis of the Upper Messinian-Lower Pliocene at the northern border of the Bajo Segura ...
En este trabajo se describen los primeros datos sobre los Osteictios de la Formación “Arcillas de Gi...
Hyperpycnal flows have been widely described in different lacustrine and marine environments but sed...