Matches in SemOpenAlex for { <https://semopenalex.org/work/W3185634164> ?p ?o ?g. }
- W3185634164 endingPage "1078" @default.
- W3185634164 startingPage "1065" @default.
- W3185634164 abstract "Abstract Cyclic strata exposed in the Inyo Mountains of eastern California contain a continuous 6 m.y. record of deep marine deposition that spans the Pennsylvanian–Permian boundary. To better understand the geologic evolution of southwest Laurentia and the role of glacially driven eustasy in upper Paleozoic stratigraphy, we measured two detailed ∼600 m composite stratigraphic sections of the Keeler Canyon Formation and collected a handheld spectral gamma ray log. Post-depositional deformation complicates field relationships, but 1:5000 scale mapping of faults and folds permits assembly of two continuous sections. Measured strata alternate at the 5–20 m scale between intervals of fine-grained laminated marlstone and intervals of mixed carbonate and siliciclastic turbidites and debrites. Based on facies characteristics and a prominent marker horizon, we reassign the Pennsylvanian-Permian age upper Salt Tram unit of the upper Keeler Canyon Formation to a new Estelle Member. We estimate sediment accumulation rates within the Keeler Canyon Formation using published conodont biostratigraphy and correlative U-Pb geochronology from Eastern Europe combined with spectral analysis and timescale optimization using the Astrochron R package. Evolutive harmonic analysis of gamma ray-derived element concentrations reveals prominent bundled periodicities that are consistent with both long and short eccentricity cycles. Average sediment accumulation rates calculated using the time scale optimization function of Astrochron suggest a gradual increase from 40–60 m/m.y. to ∼120 m/m.y. during the late Pennsylvanian and then a minima of ∼50 m/m.y. near the Pennsylvanian–Permian boundary, which is followed by an increase to ∼175 m/m.y. into the Early Permian. This trend in sediment accumulation rates and subsequent Permian contractile deformation are compatible with flexural subsidence in a SW-migrating foreland basin related to the southern part of the late Antler orogenic system." @default.
- W3185634164 created "2021-08-02" @default.
- W3185634164 creator A5001631108 @default.
- W3185634164 creator A5026243324 @default.
- W3185634164 creator A5028120769 @default.
- W3185634164 creator A5080154866 @default.
- W3185634164 date "2021-07-26" @default.
- W3185634164 modified "2023-09-25" @default.
- W3185634164 title "High-resolution late Paleozoic cyclostratigraphy and tectonic evolution of the Keeler Basin, California, southwest Laurentia" @default.
- W3185634164 cites W10540555 @default.
- W3185634164 cites W1252535697 @default.
- W3185634164 cites W1585968842 @default.
- W3185634164 cites W1589890367 @default.
- W3185634164 cites W194538708 @default.
- W3185634164 cites W1950020902 @default.
- W3185634164 cites W1966550075 @default.
- W3185634164 cites W1968139484 @default.
- W3185634164 cites W1979601663 @default.
- W3185634164 cites W1990551657 @default.
- W3185634164 cites W1994336753 @default.
- W3185634164 cites W1998138507 @default.
- W3185634164 cites W2007056514 @default.
- W3185634164 cites W2012887763 @default.
- W3185634164 cites W2018377848 @default.
- W3185634164 cites W2019003007 @default.
- W3185634164 cites W2024726427 @default.
- W3185634164 cites W2033068543 @default.
- W3185634164 cites W2035500333 @default.
- W3185634164 cites W2044198437 @default.
- W3185634164 cites W2048414881 @default.
- W3185634164 cites W2049842406 @default.
- W3185634164 cites W2055537723 @default.
- W3185634164 cites W2073986814 @default.
- W3185634164 cites W2078517319 @default.
- W3185634164 cites W2079266112 @default.
- W3185634164 cites W2088361432 @default.
- W3185634164 cites W2094196683 @default.
- W3185634164 cites W2094279940 @default.
- W3185634164 cites W2102585667 @default.
- W3185634164 cites W2119017224 @default.
- W3185634164 cites W2135909516 @default.
- W3185634164 cites W2140477756 @default.
- W3185634164 cites W2142142420 @default.
- W3185634164 cites W2143637648 @default.
- W3185634164 cites W2148251251 @default.
- W3185634164 cites W2163670123 @default.
- W3185634164 cites W2166898244 @default.
- W3185634164 cites W2482617995 @default.
- W3185634164 cites W2503219985 @default.
- W3185634164 cites W2790235851 @default.
- W3185634164 cites W2792789366 @default.
- W3185634164 cites W2793608141 @default.
- W3185634164 cites W2806299100 @default.
- W3185634164 cites W2903524071 @default.
- W3185634164 cites W2904216818 @default.
- W3185634164 cites W2952167181 @default.
- W3185634164 cites W3004112572 @default.
- W3185634164 cites W3015446400 @default.
- W3185634164 cites W3037629130 @default.
- W3185634164 cites W3110907982 @default.
- W3185634164 cites W4241679187 @default.
- W3185634164 cites W4306293736 @default.
- W3185634164 doi "https://doi.org/10.1130/b36027.1" @default.
- W3185634164 hasPublicationYear "2021" @default.
- W3185634164 type Work @default.
- W3185634164 sameAs 3185634164 @default.
- W3185634164 citedByCount "2" @default.
- W3185634164 countsByYear W31856341642023 @default.
- W3185634164 crossrefType "journal-article" @default.
- W3185634164 hasAuthorship W3185634164A5001631108 @default.
- W3185634164 hasAuthorship W3185634164A5026243324 @default.
- W3185634164 hasAuthorship W3185634164A5028120769 @default.
- W3185634164 hasAuthorship W3185634164A5080154866 @default.
- W3185634164 hasConcept C109007969 @default.
- W3185634164 hasConcept C109281948 @default.
- W3185634164 hasConcept C114793014 @default.
- W3185634164 hasConcept C126753816 @default.
- W3185634164 hasConcept C127313418 @default.
- W3185634164 hasConcept C13106087 @default.
- W3185634164 hasConcept C146588470 @default.
- W3185634164 hasConcept C149918038 @default.
- W3185634164 hasConcept C151730666 @default.
- W3185634164 hasConcept C2779004622 @default.
- W3185634164 hasConcept C2779124908 @default.
- W3185634164 hasConcept C2779650180 @default.
- W3185634164 hasConcept C30860409 @default.
- W3185634164 hasConcept C61721801 @default.
- W3185634164 hasConcept C77928131 @default.
- W3185634164 hasConcept C83365034 @default.
- W3185634164 hasConcept C84859931 @default.
- W3185634164 hasConcept C93257316 @default.
- W3185634164 hasConceptScore W3185634164C109007969 @default.
- W3185634164 hasConceptScore W3185634164C109281948 @default.
- W3185634164 hasConceptScore W3185634164C114793014 @default.
- W3185634164 hasConceptScore W3185634164C126753816 @default.
- W3185634164 hasConceptScore W3185634164C127313418 @default.
- W3185634164 hasConceptScore W3185634164C13106087 @default.
- W3185634164 hasConceptScore W3185634164C146588470 @default.