FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3081053018> ?p ?o ?g. }

• W3081053018 endingPage "340" @default.
• W3081053018 startingPage "340" @default.
• W3081053018 abstract "The Cretaceous sandstones of the Bredasdorp Basin were investigated to recognize their composition, provenance, and tectonic setting. Ninety-two samples of sandstones from exploration wells E-AH1, E-AJ1, E-BA1, E-BB1, and E-D3 were investigated using both petrographic and X-ray diffraction (XRD) methods. Petrographic studies based on quantitative investigation of the detrital framework grain shows that the Bredasdorp sandstones chiefly consist of quartz (52.2–68.0%), feldspar (10.0–18.0%), and lithic fragments (5.0–10.2%). These sandstones are mostly fine grained, moderately well-sorted, and subrounded to rounded. The modal composition data shows that the sandstones could be classified as subarkosic arenite and lithic arkose. Such a composition of the sandstones perhaps indicates the interplay of pulses of fast uplift of the source area and rapid subsidence of the Bredasdorp Basin, with subsequent periods of calmness within the transgressive-regressive sequence in a rift tectonic regime. The provenance ternary diagrams revealed that the sandstones are mainly of continental block provenances (stable shields and basement uplifted areas) and complemented by recycled sands from an associated platform. The tectonic provenance studies of Bredasdorp Basin revealed that the sandstones are typically rift sandstones and have undergone long-distance transport from the source area along the rift. In the regional context of the evolution of the Bredasdorp Basin, the results presented in this study inferred that the basin developed on a rift passive setting (trailing edge) of the stable continental margins." @default.
• W3081053018 created "2020-09-01" @default.
• W3081053018 creator A5029249550 @default.
• W3081053018 creator A5042957123 @default.
• W3081053018 creator A5051344545 @default.
• W3081053018 creator A5070365737 @default.
• W3081053018 date "2020-08-28" @default.
• W3081053018 modified "2023-09-27" @default.
• W3081053018 title "Petrography and Tectonic Provenance of the Cretaceous Sandstones of the Bredasdorp Basin, off the South Coast of South Africa: Evidence from Framework Grain Modes" @default.
• W3081053018 cites W1583523352 @default.
• W3081053018 cites W1586845937 @default.
• W3081053018 cites W192834868 @default.
• W3081053018 cites W1971124432 @default.
• W3081053018 cites W1974144393 @default.
• W3081053018 cites W1983211752 @default.
• W3081053018 cites W1986757249 @default.
• W3081053018 cites W1996312259 @default.
• W3081053018 cites W2002488699 @default.
• W3081053018 cites W2014254694 @default.
• W3081053018 cites W2021300589 @default.
• W3081053018 cites W2023601146 @default.
• W3081053018 cites W2025138594 @default.
• W3081053018 cites W2026420692 @default.
• W3081053018 cites W2040236851 @default.
• W3081053018 cites W2041876347 @default.
• W3081053018 cites W2049330470 @default.
• W3081053018 cites W2060152348 @default.
• W3081053018 cites W2064787409 @default.
• W3081053018 cites W2069851956 @default.
• W3081053018 cites W2084962457 @default.
• W3081053018 cites W2106161981 @default.
• W3081053018 cites W2164662095 @default.
• W3081053018 cites W2177791208 @default.
• W3081053018 cites W2328574824 @default.
• W3081053018 cites W2334974517 @default.
• W3081053018 cites W2767087321 @default.
• W3081053018 cites W2770429360 @default.
• W3081053018 cites W2909201321 @default.
• W3081053018 doi "https://doi.org/10.3390/geosciences10090340" @default.
• W3081053018 hasPublicationYear "2020" @default.
• W3081053018 type Work @default.
• W3081053018 sameAs 3081053018 @default.
• W3081053018 citedByCount "3" @default.
• W3081053018 countsByYear W30810530182021 @default.
• W3081053018 countsByYear W30810530182022 @default.
• W3081053018 countsByYear W30810530182023 @default.
• W3081053018 crossrefType "journal-article" @default.
• W3081053018 hasAuthorship W3081053018A5029249550 @default.
• W3081053018 hasAuthorship W3081053018A5042957123 @default.
• W3081053018 hasAuthorship W3081053018A5051344545 @default.
• W3081053018 hasAuthorship W3081053018A5070365737 @default.
• W3081053018 hasBestOaLocation W30810530181 @default.
• W3081053018 hasConcept C109007969 @default.
• W3081053018 hasConcept C12015391 @default.
• W3081053018 hasConcept C126559015 @default.
• W3081053018 hasConcept C127313418 @default.
• W3081053018 hasConcept C127413603 @default.
• W3081053018 hasConcept C138170599 @default.
• W3081053018 hasConcept C147176958 @default.
• W3081053018 hasConcept C151730666 @default.
• W3081053018 hasConcept C17409809 @default.
• W3081053018 hasConcept C2780049196 @default.
• W3081053018 hasConcept C2781297371 @default.
• W3081053018 hasConcept C41440632 @default.
• W3081053018 hasConcept C50682988 @default.
• W3081053018 hasConcept C5900021 @default.
• W3081053018 hasConcept C59235061 @default.
• W3081053018 hasConcept C77928131 @default.
• W3081053018 hasConceptScore W3081053018C109007969 @default.
• W3081053018 hasConceptScore W3081053018C12015391 @default.
• W3081053018 hasConceptScore W3081053018C126559015 @default.
• W3081053018 hasConceptScore W3081053018C127313418 @default.
• W3081053018 hasConceptScore W3081053018C127413603 @default.
• W3081053018 hasConceptScore W3081053018C138170599 @default.
• W3081053018 hasConceptScore W3081053018C147176958 @default.
• W3081053018 hasConceptScore W3081053018C151730666 @default.
• W3081053018 hasConceptScore W3081053018C17409809 @default.
• W3081053018 hasConceptScore W3081053018C2780049196 @default.
• W3081053018 hasConceptScore W3081053018C2781297371 @default.
• W3081053018 hasConceptScore W3081053018C41440632 @default.
• W3081053018 hasConceptScore W3081053018C50682988 @default.
• W3081053018 hasConceptScore W3081053018C5900021 @default.
• W3081053018 hasConceptScore W3081053018C59235061 @default.
• W3081053018 hasConceptScore W3081053018C77928131 @default.
• W3081053018 hasIssue "9" @default.
• W3081053018 hasLocation W30810530181 @default.
• W3081053018 hasOpenAccess W3081053018 @default.
• W3081053018 hasPrimaryLocation W30810530181 @default.
• W3081053018 hasRelatedWork W2012859870 @default.
• W3081053018 hasRelatedWork W2075591811 @default.
• W3081053018 hasRelatedWork W2137855335 @default.
• W3081053018 hasRelatedWork W2550412874 @default.
• W3081053018 hasRelatedWork W2909201321 @default.
• W3081053018 hasRelatedWork W3081053018 @default.
• W3081053018 hasRelatedWork W3103796482 @default.
• W3081053018 hasRelatedWork W3122516169 @default.
• W3081053018 hasRelatedWork W3138824613 @default.
• W3081053018 hasRelatedWork W4213009469 @default.

• next