How to do sequence stratigraphy in synorogenic flysch basins?

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Ashton Embry

All you can delineate are MRSs and MFSs. The MRSs are placed at the top of coarsening-upward turbidite successions with the MFSs at the top of fining-upward successions.

Grzegorz Pienkowski

Turbidite successions in synorogenic flysch basins usually reflect sediment supply and/or shore proximity/bathymetry. Careful observation of properties of the fine-grained sediments might be helpful in recognizing the most distal/deepest sediments (plus their spatial extension) and indicating important correlative surfaces (MFS). Appearance of coarser or more numerous turbidite layers is not always associated with bathymetry/shore proximity, other controlling factors are tectonics and climatic conditions in the source areas are very important because they chiefly control the sediment supply.