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- W2048820467 abstract "Abstract Grain-size distributions and sedimentary structures of Tertiary strata along Kachemak Bay indicate a variety of inchannel and overbank fluvial facies. A Markov analysis indicates cyclicity of these facies, probably caused by repeated and regular channel migration during subsidence. Fossils indicate a cool-temperate climate and probable freshwater deposition. Paleocurrent directions and sandstone composition suggest a metamorphic and sedimentary-clastic provenance during Homerian time with the addition of pyroclastics during Clamgulchian time. The Homerian Stage beds represent facies of braided-meandering streams whereas the Clamgulchian Stage beds represent facies of meandering streams. These streams flowed westward and northwestward from the Chugach-Kenai Mountains onto wooded, low-gradient, alluvial plains." @default.
- W2048820467 created "2016-06-24" @default.
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- W2048820467 date "1984-03-01" @default.
- W2048820467 modified "2023-09-27" @default.
- W2048820467 title "Environments of deposition, paleocurrents, and provenance of Tertiary deposits along Kachemak Bay, Kenai Peninsula, Alaska" @default.
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- W2048820467 doi "https://doi.org/10.1016/0037-0738(84)90088-5" @default.
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