FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2160074694> ?p ?o ?g. }

• W2160074694 endingPage "406" @default.
• W2160074694 startingPage "389" @default.
• W2160074694 abstract "ABSTRACT Petrographic and dispersal data are essential to correct interpretation of mechanisms that create continental sequence-stratigraphic architecture. A case study from southern Utah demonstrates that Upper Cretaceous (upper Santonian-Campanian) alluvial successions in the southernmost part of the Cordilleran foreland basin were deposited by fluvial systems of contrasting drainage directions and provenance, and suggests that different mechanisms governed their sequence architecture. Most of the rivers flowed northeast, subparallel to the basin foredeep. Less common fluvial systems flowed to the east-southeast. The fluvial sandstones fall naturally into four petrofacies: (1) quartzofeldspatholithic (mean Qt61F19L20); (2) feldspatholithic (Qt29F19L52); (3) quartzolithic (Qt75F6L20); and (4) quartzose (Qt99F1L1). Petrofacies 1 and 2 were derived from mixed supracrustal and basement sources to the southwest and south, respectively, whereas petrofacies 3 and 4 were derived from uplifted thrust sheets of the Sevier orogenic belt to the southwest and west, respectively. Only the east-southeast-flowing rivers transported the quartzose petrofacies. The fluvial strata, which include the uppermost Straight Cliffs, Wahweap, and Kaiparowits formations, form two large-scale stratigraphic successions typically interpreted as continental stratigraphic sequences hundreds of meters thick. Each succession begins with an amalgamated braided-fluvial deposit, grades to mudstone-rich strata with low sandstone-body connectivity, and culminates in highly connected sandstone bodies with multistory stacking. The basal amalgamated deposits of each succession are architecturally similar, but their compositional and dispersal characteristics are different. Quartzofeldspatholithic, quartzolithic, and quartzose sandstones above the lower base-level shift are variable, but generally similar in compositional and dispersal characteristics to both underlying and overlying strata, a phenomenon termed here congruence. In contrast, quartzose amalgamated fluvial sandstone above the upper base-level shift differs sharply in composition and dispersal direction from underlying and overlying lithic-rich strata. The foredeep axis controlled the progradation direction of the congruent shift, which was likely driven by climatically induced sediment influx, a eustatic fall, or both. In the case of the incongruent shift, increased sediment supply permitted the rivers to cross the foredeep. Temporal association of the upper amalgamated deposit with active structures in the thrust belt and foreland basin indicates that syntectonic thrust uplift, not isostatic uplift or climate, caused the influx of quartz." @default.
• W2160074694 created "2016-06-24" @default.
• W2160074694 creator A5014107833 @default.
• W2160074694 creator A5029722642 @default.
• W2160074694 creator A5033892402 @default.
• W2160074694 date "2003-05-01" @default.
• W2160074694 modified "2023-10-18" @default.
• W2160074694 title "Integrating Sandstone Petrology and Nonmarine Sequence Stratigraphy: Application to the Late Cretaceous Fluvial Systems of Southwestern Utah, U.S.A." @default.
• W2160074694 cites W132932171 @default.
• W2160074694 cites W138640712 @default.
• W2160074694 cites W1504446681 @default.
• W2160074694 cites W1512395851 @default.
• W2160074694 cites W1525200383 @default.
• W2160074694 cites W1579931260 @default.
• W2160074694 cites W167037963 @default.
• W2160074694 cites W1854772728 @default.
• W2160074694 cites W1929739357 @default.
• W2160074694 cites W1976568427 @default.
• W2160074694 cites W1986509574 @default.
• W2160074694 cites W2007721934 @default.
• W2160074694 cites W2012887763 @default.
• W2160074694 cites W2016223358 @default.
• W2160074694 cites W2021041237 @default.
• W2160074694 cites W2023601146 @default.
• W2160074694 cites W2033223278 @default.
• W2160074694 cites W2038699308 @default.
• W2160074694 cites W2040086201 @default.
• W2160074694 cites W2040236851 @default.
• W2160074694 cites W2045203536 @default.
• W2160074694 cites W2061533231 @default.
• W2160074694 cites W2067628429 @default.
• W2160074694 cites W2079367175 @default.
• W2160074694 cites W2083736999 @default.
• W2160074694 cites W2085675246 @default.
• W2160074694 cites W2090390688 @default.
• W2160074694 cites W2096557357 @default.
• W2160074694 cites W2099512080 @default.
• W2160074694 cites W2102264361 @default.
• W2160074694 cites W2104311334 @default.
• W2160074694 cites W2107656651 @default.
• W2160074694 cites W2109444804 @default.
• W2160074694 cites W2110366794 @default.
• W2160074694 cites W2113868045 @default.
• W2160074694 cites W2116608591 @default.
• W2160074694 cites W2117814431 @default.
• W2160074694 cites W2134491135 @default.
• W2160074694 cites W2150854303 @default.
• W2160074694 cites W2156821381 @default.
• W2160074694 cites W2158829645 @default.
• W2160074694 cites W2171430248 @default.
• W2160074694 cites W2228478404 @default.
• W2160074694 cites W2259441666 @default.
• W2160074694 cites W2263442402 @default.
• W2160074694 cites W2285820197 @default.
• W2160074694 cites W2336266680 @default.
• W2160074694 cites W2399694755 @default.
• W2160074694 cites W2466721904 @default.
• W2160074694 cites W2479174062 @default.
• W2160074694 cites W2981174554 @default.
• W2160074694 cites W3032141046 @default.
• W2160074694 cites W3129000838 @default.
• W2160074694 cites W373074925 @default.
• W2160074694 cites W42188974 @default.
• W2160074694 cites W600941587 @default.
• W2160074694 cites W2464438412 @default.
• W2160074694 cites W2525665907 @default.
• W2160074694 doi "https://doi.org/10.1306/100702730389" @default.
• W2160074694 hasPublicationYear "2003" @default.
• W2160074694 type Work @default.
• W2160074694 sameAs 2160074694 @default.
• W2160074694 citedByCount "78" @default.
• W2160074694 countsByYear W21600746942012 @default.
• W2160074694 countsByYear W21600746942013 @default.
• W2160074694 countsByYear W21600746942014 @default.
• W2160074694 countsByYear W21600746942015 @default.
• W2160074694 countsByYear W21600746942016 @default.
• W2160074694 countsByYear W21600746942017 @default.
• W2160074694 countsByYear W21600746942018 @default.
• W2160074694 countsByYear W21600746942019 @default.
• W2160074694 countsByYear W21600746942020 @default.
• W2160074694 countsByYear W21600746942021 @default.
• W2160074694 countsByYear W21600746942022 @default.
• W2160074694 crossrefType "journal-article" @default.
• W2160074694 hasAuthorship W2160074694A5014107833 @default.
• W2160074694 hasAuthorship W2160074694A5029722642 @default.
• W2160074694 hasAuthorship W2160074694A5033892402 @default.
• W2160074694 hasConcept C109007969 @default.
• W2160074694 hasConcept C109281948 @default.
• W2160074694 hasConcept C112959462 @default.
• W2160074694 hasConcept C12294951 @default.
• W2160074694 hasConcept C127313418 @default.
• W2160074694 hasConcept C146588470 @default.
• W2160074694 hasConcept C151730666 @default.
• W2160074694 hasConcept C2778112365 @default.
• W2160074694 hasConcept C42907665 @default.
• W2160074694 hasConcept C54355233 @default.
• W2160074694 hasConcept C5900021 @default.
• W2160074694 hasConcept C77928131 @default.

• next