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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Guadalupe Mountains (1)
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Permian Basin (4)
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United States
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Delaware Basin (8)
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New Mexico
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Eddy County New Mexico (2)
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Lea County New Mexico (1)
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Texas
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Andrews County Texas (1)
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Brewster County Texas (1)
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Crane County Texas (1)
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Loving County Texas (8)
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Midland Basin (1)
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Reeves County Texas (3)
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Ward County Texas (3)
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stable isotopes
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paleogeography (2)
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Paleozoic
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Permian
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Castile Formation (1)
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Guadalupian
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Brushy Canyon Formation (1)
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Lower Permian
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Leonardian
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Bone Spring Limestone (1)
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Upper Permian (1)
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petroleum (5)
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United States
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Delaware Basin (8)
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New Mexico
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Eddy County New Mexico (2)
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Lea County New Mexico (1)
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Texas
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Andrews County Texas (1)
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Brewster County Texas (1)
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Crane County Texas (1)
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Culberson County Texas (2)
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Ector County Texas (1)
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Loving County Texas (8)
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Midland Basin (1)
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Reeves County Texas (3)
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Ward County Texas (3)
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West Texas (5)
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Winkler County Texas (3)
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waste disposal (1)
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well-logging (1)
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sedimentary rocks
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sandstone (1)
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sediments
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Loving County Texas
Permeability of upper Wolfcamp lithofacies in the Delaware Basin: The role of stratigraphic heterogeneity in the production of unconventional reservoirs
Potential Poroelastic Triggering of the 2020 M 5.0 Mentone Earthquake in the Delaware Basin, Texas, by Shallow Injection Wells
Spatial and vertical patterns of peak temperature in the Delaware Basin from Raman spectroscopy of carbonaceous material
A geochemical analysis of produced water(s) from the Wolfcamp formation in the Permian Delaware Basin, western Texas
Applications of quantitative prestack seismic analysis to unconventional resource play characterization in the Permian/Delaware Basin
Parent Brine of the Castile Evaporites (Upper Permian), Texas and New Mexico
Abstract Exceptional oblique-dip exposures of submarine fan complexes of the Brushy Canyon Fm. allow reconstruction of channel geometries and reservoir architecture from the slope to the basin floor. The Brushy Canyon conslsts of 1,500 ft. of basinally restricted sandstones and siltstones that onlap older carbonate slope deposits at the NW margin of the Delaware Basin. This succession represents a lowstand qequence set comprised of lugher frequency sequences that were deposited in the basin during subaerial exposure and bypass of the adjacent carbonate shelf. Progradational sequence stacking patterns reflect changing position and character of the slope as it evolved from a relict, carbonate margin, to a constructional, siltstone-dominated slope. Lowstand fan systems tracts consist of sharp-based, laterally extensive, sand-prone basin floor deposits and large, sand-filled channels encased in siltstones on the slope. The abandonment phase of each sequence (lowstand wedge-transgressive systems tract) consists of basinward-thinning siltstones that drape the basin floor fans. The slope-tobasin distnbution of lithofacies is attributed to a three stage cycle of: 1) erosion, mass wasting, and sand bypass on the slope with concurrent deposition from sand-rich flows on the basin floor, 2) progressive backfilling of feeder channels with variable fill during waning stages of deposition, and 3) cessation of sand delivery to the basin and deposition of laterally-extensive siltstone wedges. Paleocurrents and channel distributions indicate SE-E sediment transport from the NW basin margin via closely spaced point sources.