FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2757732133> ?p ?o ?g. }

• W2757732133 endingPage "1066" @default.
• W2757732133 startingPage "1043" @default.
• W2757732133 abstract "Abstract Outcrop analogues of the Late Jurassic lower Arab‐D reservoir zone in Saudi Arabia expose a succession of fining‐upward cycles deposited on a distal middle‐ramp to outer‐ramp setting. These cycles are interrupted by erosional scours that incise up to 1·8 m into underlying deposits and are infilled with intraclasts up to boulder size (1 m diameter). Scours of similar size and infill are not commonly observed on low‐angle carbonate ramps. Outcrops have been used to characterize and quantify facies‐body geometries and spatial relationships. The coarse grain size of scour‐fills indicates scouring and boulder transport by debris or hyperconcentrated density flows strengthened by offshore‐directed currents. Longitudinal and lateral flow transformation is invoked to produce the ‘pit and wing’ geometry of the scours. Scour pits and wings erode up to 1·8 m and 0·7 m deep, respectively, and are on average 50 m wide between wing tips. The flat bases of the scours and their lack of consistent aspect ratio indicate that erosion depth was limited by the presence of cemented firmgrounds in underlying cycles. Scours define slightly sinuous channels that are consistently oriented north–south, sub‐parallel to the inferred regional depositional strike of the ramp, suggesting that local palaeobathymetry was more complex than commonly assumed. Weak lateral clustering of some scours indicates that they were underfilled and reoccupied by later scour incision and infill. Rudstone scour‐fills required reworking of material from inner ramp by high‐energy, offshore‐directed flows, associated with storm action and the hydraulic gradient produced by coastal storm setup, to generate erosion and sustain transport of clasts that are generally associated with steeper slopes. Quantitative analysis indicates that these coarse‐grained units have limited potential for correlation between wells as laterally continuous, highly permeable reservoir flow units, but their erosional and locally clustered character may increase effective vertical permeability of the Arab‐D reservoir zone as a whole." @default.
• W2757732133 created "2017-10-06" @default.
• W2757732133 creator A5000104738 @default.
• W2757732133 creator A5005324517 @default.
• W2757732133 creator A5019080744 @default.
• W2757732133 creator A5039403239 @default.
• W2757732133 creator A5039734802 @default.
• W2757732133 creator A5075368069 @default.
• W2757732133 creator A5081422106 @default.
• W2757732133 creator A5086485606 @default.
• W2757732133 creator A5086882344 @default.
• W2757732133 date "2017-12-21" @default.
• W2757732133 modified "2023-10-16" @default.
• W2757732133 title "Geometry, spatial arrangement and origin of carbonate grain-dominated, scour-fill and event-bed deposits: Late Jurassic Jubaila Formation and Arab-D Member, Saudi Arabia" @default.
• W2757732133 cites W1500064878 @default.
• W2757732133 cites W1552307154 @default.
• W2757732133 cites W1640139397 @default.
• W2757732133 cites W1927598922 @default.
• W2757732133 cites W1934469433 @default.
• W2757732133 cites W1964450983 @default.
• W2757732133 cites W1967240564 @default.
• W2757732133 cites W1972391739 @default.
• W2757732133 cites W1980748377 @default.
• W2757732133 cites W1986159477 @default.
• W2757732133 cites W1992444350 @default.
• W2757732133 cites W1998935446 @default.
• W2757732133 cites W2018000259 @default.
• W2757732133 cites W2021015288 @default.
• W2757732133 cites W2028157312 @default.
• W2757732133 cites W2028511928 @default.
• W2757732133 cites W2033816050 @default.
• W2757732133 cites W203584942 @default.
• W2757732133 cites W2038586383 @default.
• W2757732133 cites W2044690762 @default.
• W2757732133 cites W2047378475 @default.
• W2757732133 cites W2048410163 @default.
• W2757732133 cites W2053497160 @default.
• W2757732133 cites W2055412159 @default.
• W2757732133 cites W2055537723 @default.
• W2757732133 cites W2057171595 @default.
• W2757732133 cites W2057250597 @default.
• W2757732133 cites W2060471409 @default.
• W2757732133 cites W2062574513 @default.
• W2757732133 cites W2065229496 @default.
• W2757732133 cites W2071188761 @default.
• W2757732133 cites W2074708048 @default.
• W2757732133 cites W2082563398 @default.
• W2757732133 cites W2088558649 @default.
• W2757732133 cites W2090474042 @default.
• W2757732133 cites W2091134985 @default.
• W2757732133 cites W2091424027 @default.
• W2757732133 cites W2093425624 @default.
• W2757732133 cites W2095809405 @default.
• W2757732133 cites W2097033979 @default.
• W2757732133 cites W2098479229 @default.
• W2757732133 cites W2098679585 @default.
• W2757732133 cites W2104896991 @default.
• W2757732133 cites W2108511223 @default.
• W2757732133 cites W2109004561 @default.
• W2757732133 cites W2110279404 @default.
• W2757732133 cites W2113424344 @default.
• W2757732133 cites W2115997702 @default.
• W2757732133 cites W2120162798 @default.
• W2757732133 cites W2139326036 @default.
• W2757732133 cites W2149164663 @default.
• W2757732133 cites W2149854321 @default.
• W2757732133 cites W2158840115 @default.
• W2757732133 cites W2159708894 @default.
• W2757732133 cites W2161302974 @default.
• W2757732133 cites W2163315164 @default.
• W2757732133 cites W2208175532 @default.
• W2757732133 cites W2500144445 @default.
• W2757732133 cites W2607243671 @default.
• W2757732133 cites W2773138833 @default.
• W2757732133 cites W2970821525 @default.
• W2757732133 cites W2981429514 @default.
• W2757732133 cites W4241463542 @default.
• W2757732133 cites W629685990 @default.
• W2757732133 doi "https://doi.org/10.1111/sed.12414" @default.
• W2757732133 hasPublicationYear "2017" @default.
• W2757732133 type Work @default.
• W2757732133 sameAs 2757732133 @default.
• W2757732133 citedByCount "11" @default.
• W2757732133 countsByYear W27577321332018 @default.
• W2757732133 countsByYear W27577321332020 @default.
• W2757732133 countsByYear W27577321332021 @default.
• W2757732133 countsByYear W27577321332022 @default.
• W2757732133 countsByYear W27577321332023 @default.
• W2757732133 crossrefType "journal-article" @default.
• W2757732133 hasAuthorship W2757732133A5000104738 @default.
• W2757732133 hasAuthorship W2757732133A5005324517 @default.
• W2757732133 hasAuthorship W2757732133A5019080744 @default.
• W2757732133 hasAuthorship W2757732133A5039403239 @default.
• W2757732133 hasAuthorship W2757732133A5039734802 @default.
• W2757732133 hasAuthorship W2757732133A5075368069 @default.
• W2757732133 hasAuthorship W2757732133A5081422106 @default.
• W2757732133 hasAuthorship W2757732133A5086485606 @default.
• W2757732133 hasAuthorship W2757732133A5086882344 @default.

• next