1. Scales of Study
Sedimentology is performed on a number of scales from single grains
to tectonic and hydrologically-driven global sea-level cycles.
Clast
Deposit/rock
Environment/facies
System/facies association/
architectural element
Systems tract
Increasing scale and complexity
Basin
Eustatic
Sedimentology
Stratigraphy
3. Systems Tract
A systems tract consists of genetically-related (time-equivalent)
depositional systems.
4. Types of Systems Tracts
Systems tracts are divided into four categories: falling-stage, lowstand,
transgressive, and highstand, depending upon their relationship to
relative base-level change.
LowstandHighstand
9. Hanging a Section
The stratigraphic succession of a basin can be “hung” on different
horizons to distinguish the impact of different depositional events.
10. Sequence Stratigraphy
A stratigraphic sequence consists of sediment deposited during a
single cycle of sea-level fluctuation and is identified, in part, by the
presence of systems tracts representing different phases of that cycle.
Clastic Sequence Carbonate Sequence