FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1996989887> ?p ?o ?g. }

• W1996989887 abstract "The Campanian Bida Formation is the oldest stratigraphic unit in the northern Bida Basin, central Nigeria. Facies analysis of the investigated sections indicates three main facies which include conglomerate, sandstone and claystone. The poorly sorted, matrix and grain supported conglomeratic facies which overly unconformably the weathered schists and granites is interpreted as gravity induced debris flow deposit. The massive to crossbedded sandstone facies with unidirectional paleo-flow dominantly to the NNE were deposited in braided fluvial channels. The sequence grades into claystone facies which probably was formed in localized non-marine floodplains. Results of grain size analysis; standard deviation and skewness which range from 0.65 to 1.69 and -0.02 to 0.96 (average values of 1.29 and 0.11f) respectively suggest that the sandstones are predominantly texturally immature and, thus, imply fluvial origin. Average mean sizes of 0.79f suggest predominance of coarse sands and this suggest that saltation is the most prevalent mode of transportation. Pebble morphology study also indicates mainly fluvial processes for the clasts from the conglomerates and conglomeratic sandstones. Few individual clasts with sphericity and Oblate – Prolate (OP) index values less than 0.66 and -1.5 respectively, however, provide evidence of recycling of some of the clasts from older sediments. Petrographic study reveals that quartz is the dominant framework grain ranging from 66.3 to 88.5%. Feldspar dominated by plagioclase type constitutes between 10 to 27.7%. The plotted QFR diagrams suggest subarkosic sandstones derived from rifted and uplifted continental basement rocks in a warm humid paleoclimatic setting." @default.
• W1996989887 created "2016-06-24" @default.
• W1996989887 creator A5075630746 @default.
• W1996989887 date "2012-02-29" @default.
• W1996989887 modified "2023-10-03" @default.
• W1996989887 title "Depositional Environments and Petrographic Characteristics of Bida Formation around Share-Pategi, Northern Bida Basin, Nigeria" @default.
• W1996989887 cites W101633874 @default.
• W1996989887 cites W1489773112 @default.
• W1996989887 cites W1866543612 @default.
• W1996989887 cites W1978754515 @default.
• W1996989887 cites W1981723811 @default.
• W1996989887 cites W1991148604 @default.
• W1996989887 cites W2014471771 @default.
• W1996989887 cites W2023601146 @default.
• W1996989887 cites W2032902645 @default.
• W1996989887 cites W2040272737 @default.
• W1996989887 cites W2045252834 @default.
• W1996989887 cites W2052589367 @default.
• W1996989887 cites W2053403290 @default.
• W1996989887 cites W2054673645 @default.
• W1996989887 cites W2058510863 @default.
• W1996989887 cites W2074467209 @default.
• W1996989887 cites W2080591287 @default.
• W1996989887 cites W2087733602 @default.
• W1996989887 cites W2093129122 @default.
• W1996989887 cites W2097027978 @default.
• W1996989887 cites W2102272641 @default.
• W1996989887 cites W2109639559 @default.
• W1996989887 cites W2118078830 @default.
• W1996989887 cites W2119062511 @default.
• W1996989887 cites W2120934847 @default.
• W1996989887 cites W2124712922 @default.
• W1996989887 cites W2141316994 @default.
• W1996989887 cites W2154790037 @default.
• W1996989887 cites W2159525271 @default.
• W1996989887 cites W2159557178 @default.
• W1996989887 cites W2162245896 @default.
• W1996989887 cites W2162266211 @default.
• W1996989887 cites W2169555794 @default.
• W1996989887 doi "https://doi.org/10.5539/jgg.v4n1p224" @default.
• W1996989887 hasPublicationYear "2012" @default.
• W1996989887 type Work @default.
• W1996989887 sameAs 1996989887 @default.
• W1996989887 citedByCount "2" @default.
• W1996989887 countsByYear W19969898872014 @default.
• W1996989887 countsByYear W19969898872021 @default.
• W1996989887 crossrefType "journal-article" @default.
• W1996989887 hasAuthorship W1996989887A5075630746 @default.
• W1996989887 hasBestOaLocation W19969898871 @default.
• W1996989887 hasConcept C106804226 @default.
• W1996989887 hasConcept C109007969 @default.
• W1996989887 hasConcept C112959462 @default.
• W1996989887 hasConcept C114793014 @default.
• W1996989887 hasConcept C122792734 @default.
• W1996989887 hasConcept C126753816 @default.
• W1996989887 hasConcept C127313418 @default.
• W1996989887 hasConcept C138170599 @default.
• W1996989887 hasConcept C146588470 @default.
• W1996989887 hasConcept C151730666 @default.
• W1996989887 hasConcept C17409809 @default.
• W1996989887 hasConcept C2777760186 @default.
• W1996989887 hasConcept C2778520076 @default.
• W1996989887 hasConcept C2779181077 @default.
• W1996989887 hasConcept C2779870107 @default.
• W1996989887 hasConcept C5900021 @default.
• W1996989887 hasConcept C59235061 @default.
• W1996989887 hasConcept C6494504 @default.
• W1996989887 hasConceptScore W1996989887C106804226 @default.
• W1996989887 hasConceptScore W1996989887C109007969 @default.
• W1996989887 hasConceptScore W1996989887C112959462 @default.
• W1996989887 hasConceptScore W1996989887C114793014 @default.
• W1996989887 hasConceptScore W1996989887C122792734 @default.
• W1996989887 hasConceptScore W1996989887C126753816 @default.
• W1996989887 hasConceptScore W1996989887C127313418 @default.
• W1996989887 hasConceptScore W1996989887C138170599 @default.
• W1996989887 hasConceptScore W1996989887C146588470 @default.
• W1996989887 hasConceptScore W1996989887C151730666 @default.
• W1996989887 hasConceptScore W1996989887C17409809 @default.
• W1996989887 hasConceptScore W1996989887C2777760186 @default.
• W1996989887 hasConceptScore W1996989887C2778520076 @default.
• W1996989887 hasConceptScore W1996989887C2779181077 @default.
• W1996989887 hasConceptScore W1996989887C2779870107 @default.
• W1996989887 hasConceptScore W1996989887C5900021 @default.
• W1996989887 hasConceptScore W1996989887C59235061 @default.
• W1996989887 hasConceptScore W1996989887C6494504 @default.
• W1996989887 hasIssue "1" @default.
• W1996989887 hasLocation W19969898871 @default.
• W1996989887 hasOpenAccess W1996989887 @default.
• W1996989887 hasPrimaryLocation W19969898871 @default.
• W1996989887 hasRelatedWork W1538124187 @default.
• W1996989887 hasRelatedWork W1996989887 @default.
• W1996989887 hasRelatedWork W2011633203 @default.
• W1996989887 hasRelatedWork W2047143196 @default.
• W1996989887 hasRelatedWork W2061106033 @default.
• W1996989887 hasRelatedWork W2115015538 @default.
• W1996989887 hasRelatedWork W2272610183 @default.
• W1996989887 hasRelatedWork W2333933907 @default.
• W1996989887 hasRelatedWork W2612472232 @default.
• W1996989887 hasRelatedWork W2901761343 @default.
• W1996989887 hasVolume "4" @default.

• next