GEOL SED

Introducing the team sedimentary geology :

Managers : Corinne Loisy and Sébastien Zaragosi

The general objective of the team is to understand the sedimentary, structural and diagenetic processes at the origin of present and ancient sedimentary systems. It is structured around four axes and two cross-disciplinary actions.

Research areas and themes

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AXIS 1: Architecture of sedimentary basins

Coordinators : Carine Grélaud and Philippe Razin

Factors in control of the architecture of deposits in different geodynamic contexts:

  • The Meso-Cenozoic Arabian Platform, the Paleozoic North-Gondwana Platform, the Jurassic Atlas Basin, the Cretaceous-Tertiary Pyrenean basins, etc.
  • Dynamics of the ‘Apulian/Kruja Platforms – Ionian Basin’ carbonate system in the Upper Cretaceous and Palaeocene (Albania and Northern Greece).
  • Tectono-sedimentary architectures of the Upper Carboniferous-Permian basins.

 

AXIS 2: Reservoirs, Heterogeneities, Geo-fluids, Diagenesis

Coordinators : Thibault Cavailhes and Adrian Cerepi
  • Behaviour of geofluids in the context of geological storage of CO2 and energy (CH4-H2).
  • Characterisation of carbonate and volcaniclastic deposits.
  • Characterisation of authigenic carbonates on the outskirts of the Capbreton canyon.
  • Impact of micro-organisms on sandstone and carbonate diagenesis.
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AXIS 3: Processes and sedimentary environments

Coordinators : Raphaël Bourillot and Emmanuelle Ducassou
  • Study of the physical processes of sedimentation.
  • Characterisation of sedimentation at the continent-ocean interface.
  • Study of the role of micro-organisms in sedimentation.
  • Dating of sedimentary archives on a multi-decadal scale.
  • Current and recent carbonate slope morphologies.

 

AXIS 4: Geological hazard

Coordinator : Thibault Cavailhes
  • Study of seismic hazard through offshore and onshore seismogenic faults: Cycladic backarc (Milos), Karakorum, Haiti, Aquitaine basin.
  • Study of the gravity hazard through the characterisation of pillars in underground quarries and large-scale ground movements.
  • Development and evolution of offshore sinkholes.
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Cross-functional actions: Monitoring and databases

Coordinators : Corinne Loisy and Sabine Schmidt
  • To share our thoughts, experiences and methodologies relating to instrumental activities, observation and database acquisition for axes 2, 3 and 4.
  • Instrumented sites all along the Neo-Aquitaine Land-Sea Continuum support this work, including the MAGEST network, which has been observing the Gironde estuary at high frequency since 2004 (https://magest.oasu.u-bordeaux.fr/).

 

Cross-functional initiatives: Modelling

Coordinators : Carine Grélaud and Sophie Leleu

The modelling tool represents an cross-functional initiatives that cuts across the team’s 4 axes. The aim of the modelling carried out by the team or in collaboration with others is to represent the architecture of basins and reservoirs in 2D and 3D in order to correctly understand the geometry of sedimentary bodies and the parameters that control this geometry.

Equipments / Resources

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Seismic Reflection data:

Our approach is based on high-resolution (HR) seismic reflection data (Mini-GI sources and 192-channel streamers) and very high-resolution (THR) seismic data (Sparker, CHIRP, Peskavel), targeting the stratigraphy, structure, and sedimentary bodies of deep-sea, slope, and shelf environments.

These data are acquired using the resources of the French Oceanographic Fleet. Processing and interpretation are carried out in-house using Kingdom Suite®, Matlab®, and SOLID-QC (Ifremer) software.

Each year, S&P Global generously grants us 10 licenses for their seismic interpretation software, Kingdom Suite®, as part of their University Grant Program. We use Kingdom Suite® to train students in our laboratory and for the interpretation of seismic data related to our research activities. We would like to express our deep gratitude to S&P Global for this valuable opportunity.

Figure 1. Multichannel HR data. Capbreton submarine canyon – CREMER Michel (2010) SARGASS cruise, RV Pourquoi pas ?, https://doi.org/10.17600/10030080

Figure 2. CHIRP VHR data. Landes marginal plateau – CREMER Michel (2010) SARGASS cruise, RV Pourquoi pas ?, https://doi.org/10.17600/10030080