− | [[file:exploring-for-stratigraphic-traps_fig21-19.png|300px|thumb|{{figure number|1}}Three stacking patterns. From Hyne, 1995; courtesy Tulsa Geological Society. Modified from Van Wagoner et al., 1990; courtesy AAPG.]] | + | [[file:exploring-for-stratigraphic-traps_fig21-19.png|300px|thumb|{{figure number|1}}Three stacking patterns. From Hyne;<ref name=Hyne>Hyne, N. J., 1995, Sequence stratigraphy: a new look at old rocks, in N. J. Hyne, ed., Sequence Stratigraphy of the Mid Continent: Tulsa Geological Society Special Publication 4, p. 5–20.</ref> courtesy Tulsa Geological Society. Modified from Van Wagoner et al.;<ref>Van Wagoner, J. C., R. M. Mitchum, K. M. Campion, and V. D. Rahmanian, 1990, Siliciclastic Sequence Stratigraphy in Well Logs, Cores and Outcrops: Concepts for High-Resolution Correlation of Time and Facies: [http://store.aapg.org/detail.aspx?id=1196 AAPG Methods in Exploration Series No. 7], 55 p.</ref> courtesy AAPG.]] |
| Parasequences stack into [[Depocenter#Sediment_supply_rate_and_facies_patterns|three basic patterns]] as a result of the interaction of accommodation and rate of sediment supply: | | Parasequences stack into [[Depocenter#Sediment_supply_rate_and_facies_patterns|three basic patterns]] as a result of the interaction of accommodation and rate of sediment supply: |