1. Sedimentary Basin Classification

2. Miall Basin Classification
Cratonic Basins
Divergent Margin Basins
Convergent Margin Basins
Transform and Transcurrent Fault Basins
Basins Associated with Continental Collision and Suturing

3. Basin Geohistory after Kingston et al.
Basin-Forming Tectonics
Depositional Sequences
Basin-Modifying Tectonics

4. Characteristics of Basins for Kingston et al
Characteristics of Basins for Kingston et al. Classification (Basin-Forming Tectonics)
Underlying Crust Type
Type of Past Plate Movement
Basin Position on Plate

5. Basin Classification-Basin-Forming Tectonics (Kingston et al.)
Continental Basins Formed on Continental Crust
Oceanic Basins Formed on Oceanic Crust

6. Continental Basins (Kingston et al.)
Divergent Basins
Convergent Basins

7. Divergent Basins (Kingston et al.)
Continental Interior Sag Basins
Continental Interior Fracture Basins
Continental Margin Sag Basins

8. Convergent Basins (Kingston et al.)
Continental Wrench Basins
Trench Associated Basins

9. Basin Geohistory (Kingston et al.)
Basin-Forming Tectonics
Depositional Sequences
Basin-Modifying Tectonics

10. Depositional Sequences (Kingston et al.)
Non-marine Wedge Base Deposits
Marine Wedge Middle Deposits
Non-marine Wedge Top Deposits

11. Basin-Modifying Tectonics (Kingston et al.)
Episodic Wrench Faulting
Adjacent Foldbelt Development
Complete Folding of Basin Area

12. Characteristics of Cratonic Basins
Basement Structures Associated with Cratonic Movement
Plays: Traps Related to Basement Arches, Paleotopographic Features, and Stratigraphic Traps Associated with Non-marine and Shallow Marine Siliciclastics and Platform Carbonates

13. Characteristics of Divergent Margins
Interfingering of Source and Reservoir Beds
Tilting and Loading of Offshore Strata
Development of Progradational Sedimentary Wedge
Tectonic and Sedimentologic Sequence: Intracratonic, Taphrogenic, Evaporitic, Shallow Marine Platform, and Open Marine Shelf-Slope-Basin
Plays: Deep Depths (Block Faulted Basement Extensional Features Associated with Non-marine Facies, Stratigraphic Pinchouts, and Unconformities; Intermediate Depths (Salt Features Associated with Shallow Marine Facies; and Shallow Depths (Stratigraphic Traps Associated with Deltas, Reefs, and Deeper Water Sand Facies and Growth Faults

14. Divergent Margin From HGS Website, Thornton et al.

15. Characteristics of Convergent Margins
Predictability Along Strike
Better Reservoir Rock Resulting from Pluton Erosion
Basin Types: Back-Arc, Arc-Trench Gap, and Slope
Plays: Deep Depths (Vertical Tectonics, Fractured Basement Rocks, Thrusting) and Shallow Depths (Stratigraphic Traps and Unconformities Associated with Carbonate and Siliciclastic Facies)

16. Characteristics of Transform and Strike-Slip Margins
Extensional Bends Result in Basins
Plays Are Associated with En Echelon Faults and Folds, Stratigraphic Pinchouts, and Unconformities

17. Characteristics of Suture Zones
Development of Peripheral Basin and Foreland Basin
Hydrocarbons In Elevated Thermal Conditions and Driven Updip into Strata
Plays: Broad Structures of Peripheral Basin and Folds and Thrust Faults of Foreland Basin