Details
| Originalsprache | Englisch |
|---|---|
| Titel des Sammelwerks | Recent Research on Sedimentology, Stratigraphy, Paleontology, Geochemistry, Volcanology, Tectonics, and Petroleum Geology |
| Untertitel | Proceedings of the 2nd MedGU, Marrakesh 2022 (Volume 2) |
| Herausgeber/-innen | Attila Çiner, Stefano Naitza, Ahmed E. Radwan, Zakaria Hamimi, Federico Lucci, Jasper Knight, Ciro Cucciniello, Santanu Banerjee, Hasnaa Chennaoui, Domenico M. Doronzo, Carla Candeias, Jesús Rodrigo-Comino, Roohollah Kalatehjari, Afroz Ahmad Shah, Matteo Gentilucci, Dionysia Panagoulia, Helder I. Chaminé, Maurizio Barbieri, Zeynal Abiddin Ergüler |
| Herausgeber (Verlag) | Springer Nature |
| Seiten | 47-50 |
| Seitenumfang | 4 |
| ISBN (elektronisch) | 978-3-031-48758-3 |
| ISBN (Print) | 9783031487576 |
| Publikationsstatus | Veröffentlicht - 20 März 2024 |
| Veranstaltung | 2nd International conference on Mediterranean Geosciences Union, MedGU 2022 - Marrakech, Marokko Dauer: 27 Nov. 2022 → 30 Nov. 2022 |
Publikationsreihe
| Name | Advances in Science, Technology and Innovation |
|---|---|
| ISSN (Print) | 2522-8714 |
| ISSN (elektronisch) | 2522-8722 |
Abstract
The Castellón B-1, 2, 3, 4, 11, and 12 cores were studied to establish the precise age and the stratigraphic framework of the Cenozoic offshore sedimentary succession from eastern Iberia. Six stratigraphic units were recognized: (i) a Black Sandstone Unit, (ii) a Red Beds Unit, (iii) the Alcanar Conglomerates, (iv) the Tarraco “Shale,” (v) the Amposta Limestone, also known as “Amposta Chalk,” and (vi) the San Carlos Group. The Black Sandstone Unit corresponds to non-fossiliferous slightly foliated fault breccias that resemble the Carboniferous Scala Dei Formation cropping out in the Priorat area (onshore Catalonia, NE Spain). The Red Beds Unit consists of fine-grained sandstones and red clays containing Classopollis sp. pollen grains, which range from the Late Triassic to the Paleocene. According to the known stratigraphy of onshore deposits from eastern Iberia, they are comparable with the red beds of the uppermost Cretaceous-Paleocene Mediona Formation. The Alcanar Conglomerates are mainly made up of Paleozoic clasts indicating the existence of nearby subaerially exposed Paleozoic rocks. The Tarraco “Shale” is made up of siliciclastic-influenced wackestone-packstone textures with planktonic foraminifera. Above, the Amposta Limestone comprises platform carbonates rich in coralline red algae, as well as larger benthic foraminifera including Borelis sp., Heterostegina sp., Amphistegina mammilla, and Amphistegina bohdanowiczi. The foraminiferal association suggests an early-mid Langhian age. The drowning of the Amposta Limestone is marked by the deposition of the planktonic foraminifera-rich deposits of the lower part of the San Carlos Group.
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Recent Research on Sedimentology, Stratigraphy, Paleontology, Geochemistry, Volcanology, Tectonics, and Petroleum Geology: Proceedings of the 2nd MedGU, Marrakesh 2022 (Volume 2). Hrsg. / Attila Çiner; Stefano Naitza; Ahmed E. Radwan; Zakaria Hamimi; Federico Lucci; Jasper Knight; Ciro Cucciniello; Santanu Banerjee; Hasnaa Chennaoui; Domenico M. Doronzo; Carla Candeias; Jesús Rodrigo-Comino; Roohollah Kalatehjari; Afroz Ahmad Shah; Matteo Gentilucci; Dionysia Panagoulia; Helder I. Chaminé; Maurizio Barbieri; Zeynal Abiddin Ergüler. Springer Nature, 2024. S. 47-50 (Advances in Science, Technology and Innovation).
Publikation: Beitrag in Buch/Bericht/Sammelwerk/Konferenzband › Aufsatz in Konferenzband › Forschung › Peer-Review
}
TY - GEN
T1 - Sedimentary and Stratigraphic Description of the Castellón B Borehole Cores
T2 - 2nd International conference on Mediterranean Geosciences Union, MedGU 2022
AU - Bover-Arnal, Telm
AU - Ferràndez-Cañadell, Carles
AU - Aguirre, Julio
AU - Heimhofer, Ulrich
AU - Esteban, Mateu
PY - 2024/3/20
Y1 - 2024/3/20
N2 - The Castellón B-1, 2, 3, 4, 11, and 12 cores were studied to establish the precise age and the stratigraphic framework of the Cenozoic offshore sedimentary succession from eastern Iberia. Six stratigraphic units were recognized: (i) a Black Sandstone Unit, (ii) a Red Beds Unit, (iii) the Alcanar Conglomerates, (iv) the Tarraco “Shale,” (v) the Amposta Limestone, also known as “Amposta Chalk,” and (vi) the San Carlos Group. The Black Sandstone Unit corresponds to non-fossiliferous slightly foliated fault breccias that resemble the Carboniferous Scala Dei Formation cropping out in the Priorat area (onshore Catalonia, NE Spain). The Red Beds Unit consists of fine-grained sandstones and red clays containing Classopollis sp. pollen grains, which range from the Late Triassic to the Paleocene. According to the known stratigraphy of onshore deposits from eastern Iberia, they are comparable with the red beds of the uppermost Cretaceous-Paleocene Mediona Formation. The Alcanar Conglomerates are mainly made up of Paleozoic clasts indicating the existence of nearby subaerially exposed Paleozoic rocks. The Tarraco “Shale” is made up of siliciclastic-influenced wackestone-packstone textures with planktonic foraminifera. Above, the Amposta Limestone comprises platform carbonates rich in coralline red algae, as well as larger benthic foraminifera including Borelis sp., Heterostegina sp., Amphistegina mammilla, and Amphistegina bohdanowiczi. The foraminiferal association suggests an early-mid Langhian age. The drowning of the Amposta Limestone is marked by the deposition of the planktonic foraminifera-rich deposits of the lower part of the San Carlos Group.
AB - The Castellón B-1, 2, 3, 4, 11, and 12 cores were studied to establish the precise age and the stratigraphic framework of the Cenozoic offshore sedimentary succession from eastern Iberia. Six stratigraphic units were recognized: (i) a Black Sandstone Unit, (ii) a Red Beds Unit, (iii) the Alcanar Conglomerates, (iv) the Tarraco “Shale,” (v) the Amposta Limestone, also known as “Amposta Chalk,” and (vi) the San Carlos Group. The Black Sandstone Unit corresponds to non-fossiliferous slightly foliated fault breccias that resemble the Carboniferous Scala Dei Formation cropping out in the Priorat area (onshore Catalonia, NE Spain). The Red Beds Unit consists of fine-grained sandstones and red clays containing Classopollis sp. pollen grains, which range from the Late Triassic to the Paleocene. According to the known stratigraphy of onshore deposits from eastern Iberia, they are comparable with the red beds of the uppermost Cretaceous-Paleocene Mediona Formation. The Alcanar Conglomerates are mainly made up of Paleozoic clasts indicating the existence of nearby subaerially exposed Paleozoic rocks. The Tarraco “Shale” is made up of siliciclastic-influenced wackestone-packstone textures with planktonic foraminifera. Above, the Amposta Limestone comprises platform carbonates rich in coralline red algae, as well as larger benthic foraminifera including Borelis sp., Heterostegina sp., Amphistegina mammilla, and Amphistegina bohdanowiczi. The foraminiferal association suggests an early-mid Langhian age. The drowning of the Amposta Limestone is marked by the deposition of the planktonic foraminifera-rich deposits of the lower part of the San Carlos Group.
KW - Amposta Limestone
KW - Carbonate Platform
KW - Iberian Plate
KW - Miocene
KW - Western Mediterranean
UR - http://www.scopus.com/inward/record.url?scp=85189502966&partnerID=8YFLogxK
U2 - 10.1007/978-3-031-48758-3_11
DO - 10.1007/978-3-031-48758-3_11
M3 - Conference contribution
AN - SCOPUS:85189502966
SN - 9783031487576
T3 - Advances in Science, Technology and Innovation
SP - 47
EP - 50
BT - Recent Research on Sedimentology, Stratigraphy, Paleontology, Geochemistry, Volcanology, Tectonics, and Petroleum Geology
A2 - Çiner, Attila
A2 - Naitza, Stefano
A2 - Radwan, Ahmed E.
A2 - Hamimi, Zakaria
A2 - Lucci, Federico
A2 - Knight, Jasper
A2 - Cucciniello, Ciro
A2 - Banerjee, Santanu
A2 - Chennaoui, Hasnaa
A2 - Doronzo, Domenico M.
A2 - Candeias, Carla
A2 - Rodrigo-Comino, Jesús
A2 - Kalatehjari, Roohollah
A2 - Shah, Afroz Ahmad
A2 - Gentilucci, Matteo
A2 - Panagoulia, Dionysia
A2 - Chaminé, Helder I.
A2 - Barbieri, Maurizio
A2 - Ergüler, Zeynal Abiddin
PB - Springer Nature
Y2 - 27 November 2022 through 30 November 2022
ER -