By R. G. Loucks, J. Frederick Sarg
Derived from the 1991 study Symposium on Carbonate series Stratigraphy, the authors have introduced jointly in a single quantity a consultant sampling of pivotal study during this vital subject. Its 3 sections describe (1) series suggestions and sedimentologic rules, (2) seismic series case stories concerning seismic and outcrop interpretations, and (3) examples of high-frequency, meter-scale cycle deposition and stacking patterns.
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Extra info for Carbonate Sequence Stratigraphy: Recent Developments and Applications - Includes Map
_ -- --- __ --... ;,. •. • • .. _h-. ---. - - - - - � . - -� ;;� ... S6 - - - S6 S6 r L c / ExpandedHigh·Resolution High-ResolutionView View of of late Late HST HST Expanded Tie Figure16. (A) [A)AAhypothetical hypotheticalseismic seismicHne l i eacross acrossaacarbonate carbonateplatfonn platformshows showsreflections reflectionswhich whichhave havebeen been Figure interpretedto totenninale terminateby byaRlap, onlap, topJap, toplap,and anderosional erosional truncation truncationat at sequence sequenceboundar boundaries.
Thus, Thus,interpretation interpretationsuggests suggests reflections thepresence presenceof ofaa discrete discretesequence sequenceboundary boundarymarked markedby bytruncation truncationand andonlap. If, Ii, however, however,greater greaterseismic sejsmic the resolutionwere werepossible, possible,perhaps perhapsaadifferent differentinterpretation interpretationwould wouldresult. result. ls continuoussea-level sea-level fall. Instead Instead the therelative relativefaU fallisis tems interrupted by brief rises or stillstands, which can be manifested in the late highstand shelf-edge and slope interrupted by brief rises or stillstands, which can be manifested in the late highstand shelf-edge and slope stratigraphicrecord record(0 (C)as asalternating alternatingepisodes episodesof ofmass masswasting wastingand andpartial partialdepositional depositionalhealing.
1988). Furthermore, although deep-water carbonate sedi sediments may may be be introduced along some some point p i n t sources to to form fan deposits, depsits, there is aa greater tendency tendency in car- 31 3] sources of sediment to operate systems for line sourcs bonate systems toe-of-slope carbonate and form toe-of-slope carbonate aprons (Mullins (Mullins and Cook, 1986). Deposition of carbonate lowstand Cook, 1986). deposits ward thinning deposits leads to the formation of of basin basinward wedges that onlap slopes slopes and are are locally thick near the toe-of-slope.