Changes

==Interpreting parasequence sets==

==Interpreting parasequence sets==

Stratal geometries that show parasequences stacked into sets that forestep progressively toward the basin center reflect [[Depocenter#Sediment_supply_rate_and_facies_patterns|progradation]]; those that stack into sets that backstep progressively toward the basin margin reflect transgression from an increase in accommodation space that exceeds the sediment supply (Figure 4-22). Progradation of parasequence sets basinward of their age-equivalent shelf edge are, by definition, the lowstand prograding complex; parasequence sets prograding from the basin margin to the age-equivalent shelf margin may be either highstand prograding complexes or shelf margin systems tracts. The absence of a well-defined shelf/slope break complicates recognition of highstand vs. lowstand systems tracts.

Stratal geometries that show parasequences stacked into sets that forestep progressively toward the basin center reflect [[Depocenter#Sediment_supply_rate_and_facies_patterns|progradation]]; those that stack into sets that backstep progressively toward the basin margin reflect [[Wikipedia:Marine transgression|transgression]] from an increase in accommodation space that exceeds the sediment supply (Figure 4-22). Progradation of parasequence sets basinward of their age-equivalent shelf edge are, by definition, the [[Sea_level_cycle_phase_and_systems_tracts#Lowstand_systems_tracts|lowstand]] prograding complex; parasequence sets prograding from the basin margin to the age-equivalent shelf margin may be either [[Sea_level_cycle_phase_and_systems_tracts#Highstand_systems_tracts|highstand]] prograding complexes or [[Systems_tracts_and_trap_types#Shelf_margin_systems_tract_traps|shelf margin systems tracts]]. The absence of a well-defined shelf-slope break complicates recognition of highstand vs. lowstand systems tracts.

==Interpretation of stratal patterns example==

==Interpretation of stratal patterns example==