Architecture of Turbidite to Delata Basin-fill Successions: Shannon Basin, Western Ireland
Field seminar to examine seismic scale deltaic and turbidite basin fill sediment architecture.
The Namurian succession of the Shannon Basin affords an opportunity to traverse a complete basin-fill succession passing up from basin-floor turbidites, through slope deposits and into a series of deltaic cycles.
Spectacular seismic-scale coastal cliff exposures allow us to see the various geometries and processes associated with this evolving basin-fill, as well as its sequence stratigraphic architecture and syn-depositional structuration.
During this trip we will investigate a 400m-thick Upper Carboniferous (Namurian) basin-fill succession which represents the thermal subsidence phase of the Shannon Basin. This basin-fill 'megasequence' provides superb outcrop examples of:
basin-floor turbidite channels and lobe / spillover systems
turbidite sheet sands
turbidite slump sheets interbedded with channelized turbidites
major slumping associated with slope failure and healing
mud diapirs and growth faults, and their effect on river capture
incised valley fills
river dominated - wave modified delta fronts
Many of the insights to be gained here will be directly transferable to other turbidite and deltaic deposystems elsewhere in the world.
Who Should Attend
This seminar benefits both exploration and reservoir geoscientists, including geologists, geophysicists and reservoir engineers, particularly as it promotes cross discipline team building.
The trip involves moderate levels of walking and also includes a boat trip where we follow seismic / reservoir scale changes in turbidite channel architecture, continuously exposed across several kilometers in the Shannon Estuary.