Add to ORKGWave climate exerts a significant influence on the development of Holocene sedimentary prograding wedges. This is demonstrated by the fact that near-bed orbital velocities between 0.10 and 0.14 m/s (threshold for resuspension) occur in the vicinity of the infralittoral prograding wedges (IPW) offlap-breaks during storm-weather conditions, but during medium wave energy conditions in the case of prodeltaic wedges
The interaction between global (glacio- custatic sea-level rise) and regional factors (oceanographic...
A census of 83 Infralittoral Prograding Wedges (IPWs) was carried out in the Central-Eastern Tyrrhen...
Climatic changes cause alterations in circulation patterns of the world oceans. The highly saline Me...
The well-exposed systems of prograding beach ridges on the Carchuna-Calahonda (Granada) and Campo de...
A detailed facies and sequential architectural analysis has been carried out along the wedge-shaped ...
17 pages, 12 figuresPreliminary analysis of data collected during the course of a cooperative Spanis...
A combination of sedimentological, geomorphological, and pedological methods has been used to study ...
The impact of tides on the spreading of the Mediterranean Outflow Waters (MOW) in the Gulf of Cadiz ...
European Geosciences Union (EGU) General Assembly 2020, 4-8 May 2020Contourite deposits are generate...
Special issue The contourite log-book: significance for palaeoceanography, ecosystems and slope inst...
The mid-Holocene sea-level highstand is a well-known phenomenon in sea-level science, yet the knowl...
Wind-generated ocean waves drive important coastal processes that determine flooding and erosion. Oc...
A very good example of a progradational sedimentary body, the Infralittoral Prograding Wedge (IPW) h...
ABSTRACT. This paper assesses the evolution of storminess along the northern coast of the Iberian Pe...
International audienceThe sedimentation in the Gulf of Cadiz (NE Atlantic Ocean) is significantly co...
The interaction between global (glacio- custatic sea-level rise) and regional factors (oceanographic...
A census of 83 Infralittoral Prograding Wedges (IPWs) was carried out in the Central-Eastern Tyrrhen...
Climatic changes cause alterations in circulation patterns of the world oceans. The highly saline Me...
The well-exposed systems of prograding beach ridges on the Carchuna-Calahonda (Granada) and Campo de...
A detailed facies and sequential architectural analysis has been carried out along the wedge-shaped ...
17 pages, 12 figuresPreliminary analysis of data collected during the course of a cooperative Spanis...
A combination of sedimentological, geomorphological, and pedological methods has been used to study ...
The impact of tides on the spreading of the Mediterranean Outflow Waters (MOW) in the Gulf of Cadiz ...
European Geosciences Union (EGU) General Assembly 2020, 4-8 May 2020Contourite deposits are generate...
Special issue The contourite log-book: significance for palaeoceanography, ecosystems and slope inst...
The mid-Holocene sea-level highstand is a well-known phenomenon in sea-level science, yet the knowl...
Wind-generated ocean waves drive important coastal processes that determine flooding and erosion. Oc...
A very good example of a progradational sedimentary body, the Infralittoral Prograding Wedge (IPW) h...
ABSTRACT. This paper assesses the evolution of storminess along the northern coast of the Iberian Pe...
International audienceThe sedimentation in the Gulf of Cadiz (NE Atlantic Ocean) is significantly co...
The interaction between global (glacio- custatic sea-level rise) and regional factors (oceanographic...
A census of 83 Infralittoral Prograding Wedges (IPWs) was carried out in the Central-Eastern Tyrrhen...
Climatic changes cause alterations in circulation patterns of the world oceans. The highly saline Me...