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Showing 1 to 4 of 4 for “"Tidal-fluvial"”.

  1. Evolution and Architecture of an Incised Valley in the Upper Cretaceous Eagle Formation in South-Central Montana

    … boundary (SB), and transgressive surface of tidal-fluvial erosion (TSE). Within this sequence stratigraphic framework, 4 facies association, internal lower-order architectures (i.e. channel forms, lateral accretion sets, crevasse splays) and higher-order regional surfaces (i.e. sequence …

    montana-tech Repository record for Evolution and Architecture of an Incised Valley in the Upper Cretaceous Eagle Formation in South-Central Montana (opens in a new tab)

  2. Evolution and Architecture of an Incised Valley in the Upper Cretaceous Eagle Formation in South-Central Montana

    … boundary (SB), and transgressive surface of tidal-fluvial erosion (TSE). Within this sequence stratigraphic framework, 4 facies association, internal lower-order architectures (i.e. channel forms, lateral accretion sets, crevasse splays) and higher-order regional surfaces (i.e. sequence …

    montana Repository record for Evolution and Architecture of an Incised Valley in the Upper Cretaceous Eagle Formation in South-Central Montana (opens in a new tab)

  3. The sedimentology of bedforms to barforms within tidally-influenced fluvial zones (TIFZx): lower Columbia River, OR/WA, USA, and the lower Chehalis River, WA, USA

    The tidally-influenced fluvial zone (TIFZ), or ‘fluvial-tidal’ transition, is an environment characterized by unidirectional fluvial, bidirectional tidal, and oceanic oscillatory currents. TIFZ environments (i.e., deltas to estuaries) occur everywhere rivers meet ocean basins, and thus are …

    uiuc Repository record for The sedimentology of bedforms to barforms within tidally-influenced fluvial zones (TIFZx): lower Columbia River, OR/WA, USA, and the lower Chehalis River, WA, USA (opens in a new tab)

  4. Process Sedimentology and Three-Dimensional Facies Architecture of a Fluvially Dominated, Tidally Influenced Point Bar: Middle McMurray Formation, Lower Steepbank River Area, Northeastern Alberta, Canada

    … these facies are interpreted to represent a fluvially dominated, tidally influenced point bar that experienced strong seasonal variation in river discharge. Annual fluctuations between river-flood stage and low-flow stage are responsible for the deposition of fluvially dominated sand beds …

    queens Repository record for Process Sedimentology and Three-Dimensional Facies Architecture of a Fluvially Dominated, Tidally Influenced Point Bar: Middle McMurray Formation, Lower Steepbank River Area, Northeastern Alberta, Canada (opens in a new tab)