By R. G. Loucks, J. Frederick Sarg
Derived from the 1991 examine Symposium on Carbonate series Stratigraphy, the authors have introduced jointly in a single quantity a consultant sampling of pivotal examine during this very important subject. Its 3 sections describe (1) series options and sedimentologic rules, (2) seismic series case stories regarding seismic and outcrop interpretations, and (3) examples of high-frequency, meter-scale cycle deposition and stacking patterns.
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Extra resources for Carbonate Sequence Stratigraphy: Recent Developments and Applications - Includes Map
During the Holocene flooding of of the the Little Bahama Bank, some transgressive sand bodies were drowned transformed into vegetated relicts because they and transformed were not able to keep pace with rising sea level (Hine, 1977). 1977). We have not seen any documentation of of the lowstand and transgressive succession of of lithofacies in andent ancient rimmed rimmed shelf shelf margins, but a hYJXlthetical hypothetical example is offered in Figure Figure 14. 14. , 1988). 1988). During During this interval of of time, shallow-marine sedimen sedimentation rates commonly exceed subsidence and the aggradato deposition of aggrada ead i ng 10 deposilion of eustatic rise, thus lleading tional tional to progradational shelf, shelf-edge, shelf-edge, and slope 1988).
Hydrocarbons. When When used in in conjunction conjunction with seismic seismic records, records, well well logs, logs, and and core core data, data, the the models may may be be applied. applied carefully carefuliy to to specific specificcase case stud studies to to help help delineate delineate reservoir-, reservoir-, seai-, seaI-, and and SOUTce sourceprone facies. facies. Caution Caution must must be be exercised, exercised, however, however, because because the the models models are are not templates templates that that can can be applied applied rigidly rigidly to to any any platform, platform, modern modern or or ancient.
In In the former dormer casc, case, carbonate carbonate clasts may mag originate from reworking of hardgrounds, cemented burrows, and and reef-crest reef-crest of and -flat boundstone clasts. Tn chsts In the latter case, clasts are rcworkcd from caliche crusts, crusts. supratidal suoratidal and arc reworked from intertidal intcrtida1 mudflats, mud flats, intertidal beachrock beachroci layers, Iayers, and water-table hardgrounds. hardgrounds. , tidal tidal flats, islands, coastal coastal dunes, and beaches), beaches), and their subsequent subsequent erosion erosion by shore shoreline retreat.