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- W1969374502 abstract "The Lower to Middle(?) Triassic Red Peak and Crow Mountain Formations of central Wyoming have commonly been interpreted as being of shallow marine or shelf origin. This paper presents conclusive evidence of an aeolian origin for parts of the two formations. The interpretation is based on highly indicative sedimentary structures including wind ripple, grainfall and grainflow strata, lag deposits, and granule ripples in the sediments of these formations. Facies in the upper Red Peak and lower Crow Mountain Formations represent aeolian dune, sandsheet, wet interdune and sabkha environments. Emphasis is placed on the recognition and interpretation of correlative surfaces of regional extent, which not only allow subdivision of the aeolian sediments into different genetic sequences, but also aid in the reconstruction of the depositional history. The recognition of an aeolian deposystem and of regional bounding surfaces adds valuable information to the efforts of reconstructing the Triassic paleogeography of the Western Interior." @default.
- W1969374502 created "2016-06-24" @default.
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- W1969374502 date "2000-04-01" @default.
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- W1969374502 title "Aeolian sediments in lower to middle (?) Triassic rocks of central Wyoming" @default.
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- W1969374502 doi "https://doi.org/10.1016/s0037-0738(99)00129-3" @default.
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