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• W2810340000 endingPage "837" @default.
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• W2810340000 abstract "Abstract The Middle Jurassic Todilto Member of the Wanakah Formation is a carbonate and gypsum unit inset into the underlying aeolian Entrada Sandstone in the San Juan Basin. Field and thin section study of the uppermost Entrada and Todilto at Ghost Ranch, New Mexico, identified Todilto facies and their relationship to remnant Entrada dune topography. Results support the previous interpretation that the Entrada dunes, housed in a basin below sea level, were rapidly flooded by marine waters. Mass wasting of the dunes gave rise to sediment‐gravity flows that largely buried remnant dune topography, leaving ca 12 m of relief that defined the antecedent condition for Todilto deposition. Previously interpreted as seasonal varves deposited in a stratified water body, the Todilto is reinterpreted as a microbial biolaminite. Most diagnostic are organic‐rich laminae with structures characteristic of filamentous microbes and containing trapped aeolian silt, and clotted‐texture laminae with a fabric associated with calcification of extracellular polymeric substances. The spatial arrangement of Todilto facies is controlled by the dune palaeotopography. A continuous basal laminated mudstone thickens over the dune crest, reflecting the optimum conditions for microbial mat development, and is interpreted to have been deposited when marine waters submerged the topography. Subsequent drying caused emergence of the crestal area, and formation of tepee structures and a dissolution breccia. Gypsiferous mudflats and periodic ponds occupied the dune flanks and interdune area, with gypsum concentrated within the interdune area. Entrada sands remained unstable during Todilto deposition with common injection structures into the Todilto, and a remnant slope caused the downslope movement and folding of Todilto strata on the upper lee face. Although some expansion of the gypsum occurred in the subsurface, facies architecture fostered development of a dissolution front adjacent to the interdune gypsum body with section collapse of gypsiferous limestone on the dune flanks." @default.
• W2810340000 created "2018-07-10" @default.
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• W2810340000 date "2018-09-22" @default.
• W2810340000 modified "2023-10-18" @default.
• W2810340000 title "Antecedent aeolian dune topographic control on carbonate and evaporite facies: Middle Jurassic Todilto Member, Wanakah Formation, Ghost Ranch, New Mexico, USA" @default.
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• W2810340000 cites W1589890367 @default.
• W2810340000 cites W1757052698 @default.
• W2810340000 cites W1943818108 @default.
• W2810340000 cites W1963488633 @default.
• W2810340000 cites W1965380953 @default.
• W2810340000 cites W1968708864 @default.
• W2810340000 cites W1972903976 @default.
• W2810340000 cites W1974110480 @default.
• W2810340000 cites W1984007724 @default.
• W2810340000 cites W1993131012 @default.
• W2810340000 cites W1993734501 @default.
• W2810340000 cites W1994327056 @default.
• W2810340000 cites W1995185494 @default.
• W2810340000 cites W1998555435 @default.
• W2810340000 cites W2000940771 @default.
• W2810340000 cites W2008934762 @default.
• W2810340000 cites W2013403815 @default.
• W2810340000 cites W2013428409 @default.
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• W2810340000 cites W2024488818 @default.
• W2810340000 cites W2028276954 @default.
• W2810340000 cites W2033444063 @default.
• W2810340000 cites W2045012505 @default.
• W2810340000 cites W2046804497 @default.
• W2810340000 cites W2047451536 @default.
• W2810340000 cites W2049404049 @default.
• W2810340000 cites W2050713785 @default.
• W2810340000 cites W2070797254 @default.
• W2810340000 cites W2070944562 @default.
• W2810340000 cites W2071197154 @default.
• W2810340000 cites W2086913906 @default.
• W2810340000 cites W2095279866 @default.
• W2810340000 cites W2096522903 @default.
• W2810340000 cites W2101477926 @default.
• W2810340000 cites W2102135244 @default.
• W2810340000 cites W2104777960 @default.
• W2810340000 cites W2110159066 @default.
• W2810340000 cites W2116781939 @default.
• W2810340000 cites W2118124391 @default.
• W2810340000 cites W2132914584 @default.
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• W2810340000 cites W2139323869 @default.
• W2810340000 cites W2142539052 @default.
• W2810340000 cites W2145154988 @default.
• W2810340000 cites W2150772200 @default.
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• W2810340000 cites W2318042047 @default.
• W2810340000 cites W2332732222 @default.
• W2810340000 cites W2535713160 @default.
• W2810340000 cites W2763447466 @default.
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• W2810340000 doi "https://doi.org/10.1111/sed.12518" @default.
• W2810340000 hasPublicationYear "2018" @default.
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