Add to ORKGThe stratigraphie framework of the non-marine Upper Eocene-Lower Oligocene in the Eastern Ebro Basin (Igualada-Sta. Coloma de Queralt area) is characterized by three main lithostratigraphic assemblages. The lower assemblage (Upper Eocene) comprises units mainly formed by alluvial deposits. The intermediate assemblage (Lowermost Oligocene) is formed by units wich originated in lacustrine environments. The upper assemblage (Lower Oligocene) comprises units formed by lacustrine and fluviolacustrine deposits. The main lithologic features of the units which constitute this stratigraphic framework are describe
An important evaporitic sedimentation occurred during the Paleogene (Eocene to lower Oligocene) in t...
Four main unconformities (1–4) were recognized in the sedimentary record of the Cenozoic basins of ...
An important evaporitic sedimentation occurred during the Paleogene (Eocene to lower Oligocene) in t...
The stratigraphic framework of the non-marine Upper Eocene-Lower Oligocene in the Eastern Ebro Basi ...
This paper deals with new data on the lithostratigraphy of the Upper Paleocene-Lower Oligocene succe...
This paper deal with new data on the lithostratigraphy of the Upper Paleocene-Lower Oligocene succes...
Some unknown stratigraphical and structural characteristics of the lower Tertiary Ebro Basin infill ...
The stratigraphic basis of this work has allowed the use of larger foraminifers in the biostratigrap...
The stratigraphic basis of this work has allowed the use of larger foraminifers in the biostratigrap...
This project has focused on the Early and Middle Eocene sediments of the Pamplona Basin, an area whi...
International audienceThe Eocene to Oligocene sediments of the Ecuadorian Oriente Basin record two k...
In the southeastern Ebro Foreland Basin, the marine deposits of Lutetian and Bartonian age show exce...
The Eocene sequence along the central part of the SE margin of the Tertiary Ebro Basin (Igualada are...
The Paleogene Alicante Trough of the South-Iberian Margin (External Betic Zone) consists of a narrow...
The Paleogene Alicante Trough of the South-Iberian Margin (External Betic Zone) consists of a narrow...
An important evaporitic sedimentation occurred during the Paleogene (Eocene to lower Oligocene) in t...
Four main unconformities (1–4) were recognized in the sedimentary record of the Cenozoic basins of ...
An important evaporitic sedimentation occurred during the Paleogene (Eocene to lower Oligocene) in t...
The stratigraphic framework of the non-marine Upper Eocene-Lower Oligocene in the Eastern Ebro Basi ...
This paper deals with new data on the lithostratigraphy of the Upper Paleocene-Lower Oligocene succe...
This paper deal with new data on the lithostratigraphy of the Upper Paleocene-Lower Oligocene succes...
Some unknown stratigraphical and structural characteristics of the lower Tertiary Ebro Basin infill ...
The stratigraphic basis of this work has allowed the use of larger foraminifers in the biostratigrap...
The stratigraphic basis of this work has allowed the use of larger foraminifers in the biostratigrap...
This project has focused on the Early and Middle Eocene sediments of the Pamplona Basin, an area whi...
International audienceThe Eocene to Oligocene sediments of the Ecuadorian Oriente Basin record two k...
In the southeastern Ebro Foreland Basin, the marine deposits of Lutetian and Bartonian age show exce...
The Eocene sequence along the central part of the SE margin of the Tertiary Ebro Basin (Igualada are...
The Paleogene Alicante Trough of the South-Iberian Margin (External Betic Zone) consists of a narrow...
The Paleogene Alicante Trough of the South-Iberian Margin (External Betic Zone) consists of a narrow...
An important evaporitic sedimentation occurred during the Paleogene (Eocene to lower Oligocene) in t...
Four main unconformities (1–4) were recognized in the sedimentary record of the Cenozoic basins of ...
An important evaporitic sedimentation occurred during the Paleogene (Eocene to lower Oligocene) in t...