FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2287111010> ?p ?o ?g. }

• W2287111010 endingPage "134" @default.
• W2287111010 startingPage "77" @default.
• W2287111010 abstract "ABSTRACT The Permian-Triassic Khuff Formation crops out in central Saudi Arabia along a N-S belt, some 1,200 km in length. It is 171.4 m (562.2 ft) thick in the type section and divided into five members; from oldest to youngest: Ash Shiqqah (formerly Unayzah member of the Khuff Formation), Huqayl, Duhaysan, Midhnab and Khartam. The base of the Khuff Formation is recognised as a regional unconformity (Pre-Khuff Unconformity), and the top of the formation is defined by the conformable contact with the overlying Sudair Shale. The Ash Shiqqah Member is tentatively dated as ?Middle Permian ?Capitanian (?Midian) based on the presence of the fusulinids Monodiexodina kattaensis and Reichelina sp. The Huqayl Member is tentatively dated as ?Late Permian ?Wuchiapingian (?Dzhulfian) based on an assemblage of smaller foraminifers dominated by Pseudomidiella cf. labensis, Earlandia? spp. and Neodiscus aff. qinglongensis. The Duhaysan Member is dated as Late Permian (Wuchiapingian-Changhsingian) based on Hemigordius baoqingensis, Graecodiscus cf. kotlyarae, “Dentalina” hoi, and Colaniella cf. minuta. The sMidhnab Member is dated as Changhsingian (Dorashamian) based on Paradagmarita sp. and “Glomospirella spirillinoides” and the disappearance of the genera Nankinella and Globivalvulina. Within the continental facies in the upper part of the Midhnab Member, incised channels facies yielded the Late Permian Midhnab Flora. The Lower Khartam Member is also dated as latest Permian (Dorashamian) based on the presence of several species of Paradagmarita and “Nodosaria” dzhulfensis in the lowest beds of the member, and the ostracods Paraparchites spp., Knoxiella spp. and Kloedenellitina sp. throughout the Lower Khartam Member. The Upper Khartam Member is assigned to an Early Triassic (‘Scythian’) age based on the occurrence of the characteristic annelid Spirorbis phlyctaena. The Khuff Formation, in central Saudi Arabian outcrops, consists of four regional depositional sequences (DS PKh, DS PKm, DS PKk and DS TrS), each containing a maximum flooding interval (MFI, with the same designation). The oldest sequence DS PKh (named after Permian-Khuff-Huqayl) consists of the Ash Shiqqah and overlying Huqayl members. The basal sequence boundary corresponds to the Pre-Khuff Unconformity (PKU) and represents the onset of the first Permian flooding event recorded in the outcrops of Saudi Arabia. The massive gypsum, gypsiferous claystone, and solution breccias in the Ash Shiqqah Member are correlated to the subsurface Khuff-D Anhydrite. The MFI PKh is positioned in the basal part of the Huqayl Member, and is followed by the regressive evaporitic palaeoenvironments of the Huqayl Member. The DS PKm (named after Permian-Khuff-Midhnab) starts with the subtidal to littoral deposits of the Duhaysan Member, over an erosive surface upon DS PKh; and ends with the regressive supratidal to continental deposits at the upper part of the Midhnab Member. The MFI PKm is located at the base of the Midhnab Member, where limestones yielded an abundant marine fauna including cephalopods and brachiopods. The terminal Permian DS PKk (Permian-Khuff-Khartam) corresponds to the Lower Khartam Member. The basal SB PKk is marked by a return to marine subtidal conditions after the continental break at the end of DS PKm. The MFI PKk is characterised by marine fauna including abundant Permian ostracods, bactritids, and locally cephalopods. The DS TrS (named after the Sudair Shale Formation) starts with the littoral, tidal to intertidal deposits of the Early Triassic Upper Khartam Member of the Khuff Formation, and ends with the closed basin, clayey to evaporitic rocks of the Early Triassic Sudair Shale." @default.
• W2287111010 created "2016-06-24" @default.
• W2287111010 creator A5019328510 @default.
• W2287111010 creator A5021604188 @default.
• W2287111010 creator A5022478113 @default.
• W2287111010 creator A5038965329 @default.
• W2287111010 creator A5054427253 @default.
• W2287111010 creator A5055304725 @default.
• W2287111010 creator A5066243148 @default.
• W2287111010 creator A5081811780 @default.
• W2287111010 creator A5088712897 @default.
• W2287111010 date "2005-10-01" @default.
• W2287111010 modified "2023-10-15" @default.
• W2287111010 title "The Permian-Triassic Khuff Formation of central Saudi Arabia" @default.
• W2287111010 cites W1580174060 @default.
• W2287111010 cites W159079554 @default.
• W2287111010 cites W1970818951 @default.
• W2287111010 cites W1986107162 @default.
• W2287111010 cites W1988398424 @default.
• W2287111010 cites W2006751098 @default.
• W2287111010 cites W2041622963 @default.
• W2287111010 cites W2053154125 @default.
• W2287111010 cites W2053493272 @default.
• W2287111010 cites W2054921342 @default.
• W2287111010 cites W2069467375 @default.
• W2287111010 cites W2085188216 @default.
• W2287111010 cites W2127288366 @default.
• W2287111010 cites W2139711367 @default.
• W2287111010 cites W2191182709 @default.
• W2287111010 cites W2313285032 @default.
• W2287111010 cites W2327228832 @default.
• W2287111010 cites W2910362007 @default.
• W2287111010 cites W2944320642 @default.
• W2287111010 cites W2954113145 @default.
• W2287111010 cites W2968599283 @default.
• W2287111010 cites W2969747300 @default.
• W2287111010 cites W2979942938 @default.
• W2287111010 cites W2986225371 @default.
• W2287111010 cites W2996108273 @default.
• W2287111010 cites W3127056474 @default.
• W2287111010 cites W4232328127 @default.
• W2287111010 cites W88175743 @default.
• W2287111010 doi "https://doi.org/10.2113/geoarabia100477" @default.
• W2287111010 hasPublicationYear "2005" @default.
• W2287111010 type Work @default.
• W2287111010 sameAs 2287111010 @default.
• W2287111010 citedByCount "69" @default.
• W2287111010 countsByYear W22871110102012 @default.
• W2287111010 countsByYear W22871110102013 @default.
• W2287111010 countsByYear W22871110102014 @default.
• W2287111010 countsByYear W22871110102015 @default.
• W2287111010 countsByYear W22871110102016 @default.
• W2287111010 countsByYear W22871110102017 @default.
• W2287111010 countsByYear W22871110102018 @default.
• W2287111010 countsByYear W22871110102019 @default.
• W2287111010 countsByYear W22871110102020 @default.
• W2287111010 countsByYear W22871110102021 @default.
• W2287111010 countsByYear W22871110102022 @default.
• W2287111010 countsByYear W22871110102023 @default.
• W2287111010 crossrefType "journal-article" @default.
• W2287111010 hasAuthorship W2287111010A5019328510 @default.
• W2287111010 hasAuthorship W2287111010A5021604188 @default.
• W2287111010 hasAuthorship W2287111010A5022478113 @default.
• W2287111010 hasAuthorship W2287111010A5038965329 @default.
• W2287111010 hasAuthorship W2287111010A5054427253 @default.
• W2287111010 hasAuthorship W2287111010A5055304725 @default.
• W2287111010 hasAuthorship W2287111010A5066243148 @default.
• W2287111010 hasAuthorship W2287111010A5081811780 @default.
• W2287111010 hasAuthorship W2287111010A5088712897 @default.
• W2287111010 hasBestOaLocation W22871110101 @default.
• W2287111010 hasConcept C109007969 @default.
• W2287111010 hasConcept C127313418 @default.
• W2287111010 hasConcept C146588470 @default.
• W2287111010 hasConcept C151730666 @default.
• W2287111010 hasConcept C153127940 @default.
• W2287111010 hasConcept C191735495 @default.
• W2287111010 hasConcept C2781229967 @default.
• W2287111010 hasConcept C83365034 @default.
• W2287111010 hasConceptScore W2287111010C109007969 @default.
• W2287111010 hasConceptScore W2287111010C127313418 @default.
• W2287111010 hasConceptScore W2287111010C146588470 @default.
• W2287111010 hasConceptScore W2287111010C151730666 @default.
• W2287111010 hasConceptScore W2287111010C153127940 @default.
• W2287111010 hasConceptScore W2287111010C191735495 @default.
• W2287111010 hasConceptScore W2287111010C2781229967 @default.
• W2287111010 hasConceptScore W2287111010C83365034 @default.
• W2287111010 hasIssue "4" @default.
• W2287111010 hasLocation W22871110101 @default.
• W2287111010 hasLocation W22871110102 @default.
• W2287111010 hasLocation W22871110103 @default.
• W2287111010 hasOpenAccess W2287111010 @default.
• W2287111010 hasPrimaryLocation W22871110101 @default.
• W2287111010 hasRelatedWork W1974744679 @default.
• W2287111010 hasRelatedWork W2113608457 @default.
• W2287111010 hasRelatedWork W2142847233 @default.
• W2287111010 hasRelatedWork W2252477519 @default.
• W2287111010 hasRelatedWork W2300470929 @default.
• W2287111010 hasRelatedWork W2363506073 @default.

• next