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- W358448263 abstract "Sauk platform carbonates of the northern Appalachian passive (Gondwana) margin are composed of high-frequency stacking patterns containing fifth-order depositional cycles. Most of the these cycles, termed parasequences in this study, display upward-shoaling peritidal patterns, commonly terminating in emergence. Parasequence surfaces are erosional resulting from this emergence and have associated karst features, especially solution-collapse breccia. The carbonates, mostly fine- to medium-crystalline and locally vuggy dolostones, are generally of low permeability. Solution-collapse breccias increase whole-rock penneability through fractures. In addition to solution-collapse breccias, emergence generated terra-ross a soil, now lithified, as well as silcrete, now chert, and caused the dedolomitization of dolostones, Upward-coarsening facies cycles, in which flat-pebble conglomerates overlie erosional surfaces, are thought to be storm generated. Yetstorm deposits with intraclasts sufficiently angular to be termed breccia may also terminate parasequences. Rfth-order upward-shoaling peritidal parasequences may be the result of extraterrestrial forcing or tectonic events causing rapid eustatic or relative changes in sea-level, respectively. Hence porosity-permeability development may likewise relate to these mechanisms. During the Sank interval anomalous storm periods may have held sway on a global scale and generated upward-coarsen ing parasequences. Storm-weather periods probably resulted from astronomical changes (extraterrestrial forcing). Porosity and per meability in the storm deposits may also be controlled by extraterrestrial forcing functions." @default.
- W358448263 created "2016-06-24" @default.
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- W358448263 date "1994-01-01" @default.
- W358448263 modified "2023-09-27" @default.
- W358448263 title "UPPER CAMBRIAN-LOWERORDOVICIAN (SAUK) PLATFORM CARBONATESOF THE NORTHERN APPALACHIAN(GONDWANA) PASSIVEMARGIN" @default.
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