SESSIONS

Contributions to every topic related to the process sedimentology, stratigraphy, paleoenvironments, geophysical, geochemical and petrophysical methods on sediments and sedimentary rocks, applied sedimentology and other fields are welcome. The focus of the meeting will be on plenary sessions rather than a number of parallel sessions, in order to promote scientific communication across barriers separating specialized fields.

SESSIONS

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Contributions to every topic related to the process sedimentology, stratigraphy, paleoenvironments, geophysical, geochemical and petrophysical methods on sediments and sedimentary rocks, applied sedimentology and other fields are welcome. The focus of the meeting will be on plenary sessions rather than a number of parallel sessions, in order to promote scientific communication across barriers separating specialized fields. Authors are invited to submit their papers into one of four sessions. The papers can be presented either orally or as poster presentations. The scientific committee will reserve the right to decide about oral or poster presentation of the submitted papers.

  1. Clastic depositional systems: processes and controls
    Understanding the behaviour of clastic systems, from mountain catchments to deep sea fans, requires study of modern environments, experimental work, interpretation of seismic datasets, as well as classical field work.  The focus of this session is on the analysis and interpretation of clastic sedimentary bodies on all scales relevant to process-oriented sedimentologists as well as to sequence stratigraphers. Case histories from fossil and modern record as well as conceptual and experimental contributions are welcome.
     
  2. Sedimentary archives of environmental changes from Neogene to Anthropocene
    This section will put together researchers documenting past environmental changes in sedimentary records of high temporal resolution and/or long temporal extent. Particularly welcome are contributions combining several approaches to reconstruct the past environments. The focus will be on climate/environmental changes on Milankovitch as well as sub-Milankovitch timescales down through to millennia and centuries. In case of Holocene environmental/climate change, with increasing human influence, studies of the impact of human presence in changing sedimentary environments, biota, or chemical pollution will be an important complement to more traditional sedimentological approaches.
     
  3. Reading the deep-time sedimentary record: stratigraphy across depositional systems and time slicesProgress in correlation and interpretation of deep-time (~pre Cenozoic) sedimentary record is one of the big challenges in the science of stratigraphy. Searching for new correlative tools and extending the actualistic concepts of astronomic tuning, chemostratigraphy, oceanographic overturns, climate change, etc. into the Mesozoic and Palaeozoic represent the cutting edges of current stratigraphic efforts, both in the industry and academia. This session will be devoted to analysis of pre-Cenozoic sedimentary record from all types of depositional systems including carbonates, evaporites and siliciclastics. Authors are invited to present contributions utilizing a broad range of methods from traditional facies analysis to multiproxy studies involving geochemical, geophysical and petrophysical data.
     
  4. Sedimentary record of tectonic and geodynamic evolution of Central Europe 
    This section will focus on tectonic signature in sedimentary record and the analysis of sedimentary basins in the Central European region. From the Neoproterozoic to late Cenozoic, major orogenies, Cadomian, Caledonian, Variscan and Alpine contributed to the building of the Central European lithosphere, resulting in overwhelming variability of past and present-day mountain belts and adjacent sedimentary basins. The response of sedimentary systems to tectonics will be the focus of this session. Contributions covering facies analysis, provenance studies, subsidence and thermal history, tectonic geomorphology and diagenetic history, and utilizing a range of datasets including field data, geophysics, geochemistry and petrophysics, are welcome.