FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2300959400> ?p ?o ?g. }

• W2300959400 endingPage "1020" @default.
• W2300959400 startingPage "1009" @default.
• W2300959400 abstract "Exposures of the Early Pliocene Waindalithi Conglomerate are confined to no more than a dozen scattered outcrops in the northeast part of Viti Levu, the main island of the Fijian archipelago. The Waindalithi Conglomerate is waterlain, but its sedimentology is unlike that expected either in debris flow deposits or in sediments entrained by conventional fluvial processes. Instead, the unit is likely to represent deposition from hyperconcentrated flows. Deposits of this sort have probably been under-identified in the rock record. In part, this is because no single characteristic is diagnostic of hyperconcentrated flow deposition. A combination of gravel lithology, sedimentary fabric, particle-size distribution and the sedimentology of individual beds proved valuable for the recognition of these deposits in this work. The deposition of the Waindalithi Conglomerate appears to have been immediately predated by a significant episode of volcanicity along the Nakauvadra and Nakorotubu ranges to the north of the region. Several eruptive centres may be recognised in the ranges, including the 25 km-diameter Rakiraki Volcano and the newly identified Nadelanadro, Namarai, Tova and Naimasi volcanoes. Fan-like masses of volcanic conglomerate drape the southern flanks of the ranges. Southerly drainage down these fans was diverted east along the gutter developed where the fans abutted the ridge-and-vale topography of the Wainibuka and Matailombau hills. Downstream, the drainage resumed its southerly course via the topographic outlet of the Wainibuka gap and onto the coastal lowlands of the Early Pliocene sea. The Waindalithi Conglomerate forms a fan-like sediment body at the southern end of the gap. While the basal components of the Waindalithi Conglomerate may have been laid down under terrestrial conditions, the upper elements may have been deposited in shallow marine conditions, with the environment of deposition changing over time as local sea-levels rose." @default.
• W2300959400 created "2016-06-24" @default.
• W2300959400 creator A5008595951 @default.
• W2300959400 creator A5052685531 @default.
• W2300959400 date "2015-11-17" @default.
• W2300959400 modified "2023-09-26" @default.
• W2300959400 title "The stratigraphy and sedimentology of the Waindalithi Conglomerate of northeast Viti Levu, Fiji: hyperconcentrated flows and Pliocene environmental history" @default.
• W2300959400 cites W1496365707 @default.
• W2300959400 cites W1576572213 @default.
• W2300959400 cites W1974792361 @default.
• W2300959400 cites W1979002005 @default.
• W2300959400 cites W1990436032 @default.
• W2300959400 cites W2000108132 @default.
• W2300959400 cites W2004529964 @default.
• W2300959400 cites W2008719431 @default.
• W2300959400 cites W2019438003 @default.
• W2300959400 cites W2039236487 @default.
• W2300959400 cites W2040771943 @default.
• W2300959400 cites W2056643310 @default.
• W2300959400 cites W2064972007 @default.
• W2300959400 cites W2069244670 @default.
• W2300959400 cites W2079335325 @default.
• W2300959400 cites W2102017033 @default.
• W2300959400 cites W2107632118 @default.
• W2300959400 cites W2117792414 @default.
• W2300959400 cites W2127132152 @default.
• W2300959400 cites W2139417932 @default.
• W2300959400 cites W2156945129 @default.
• W2300959400 cites W2159525271 @default.
• W2300959400 cites W2166344568 @default.
• W2300959400 cites W2172081334 @default.
• W2300959400 cites W2503823564 @default.
• W2300959400 cites W2540840598 @default.
• W2300959400 cites W2974884155 @default.
• W2300959400 cites W4237867004 @default.
• W2300959400 cites W2076962759 @default.
• W2300959400 doi "https://doi.org/10.1080/08120099.2015.1127857" @default.
• W2300959400 hasPublicationYear "2015" @default.
• W2300959400 type Work @default.
• W2300959400 sameAs 2300959400 @default.
• W2300959400 citedByCount "3" @default.
• W2300959400 countsByYear W23009594002017 @default.
• W2300959400 countsByYear W23009594002019 @default.
• W2300959400 countsByYear W23009594002022 @default.
• W2300959400 crossrefType "journal-article" @default.
• W2300959400 hasAuthorship W2300959400A5008595951 @default.
• W2300959400 hasAuthorship W2300959400A5052685531 @default.
• W2300959400 hasBestOaLocation W23009594002 @default.
• W2300959400 hasConcept C104873425 @default.
• W2300959400 hasConcept C106804226 @default.
• W2300959400 hasConcept C109007969 @default.
• W2300959400 hasConcept C109281948 @default.
• W2300959400 hasConcept C111368507 @default.
• W2300959400 hasConcept C112959462 @default.
• W2300959400 hasConcept C114793014 @default.
• W2300959400 hasConcept C120806208 @default.
• W2300959400 hasConcept C122792734 @default.
• W2300959400 hasConcept C127313418 @default.
• W2300959400 hasConcept C127491152 @default.
• W2300959400 hasConcept C151730666 @default.
• W2300959400 hasConcept C17409809 @default.
• W2300959400 hasConcept C185933670 @default.
• W2300959400 hasConcept C18903297 @default.
• W2300959400 hasConcept C20470049 @default.
• W2300959400 hasConcept C23389524 @default.
• W2300959400 hasConcept C2776023875 @default.
• W2300959400 hasConcept C2776643431 @default.
• W2300959400 hasConcept C2816523 @default.
• W2300959400 hasConcept C64297162 @default.
• W2300959400 hasConcept C6494504 @default.
• W2300959400 hasConcept C65589250 @default.
• W2300959400 hasConcept C77928131 @default.
• W2300959400 hasConcept C86803240 @default.
• W2300959400 hasConceptScore W2300959400C104873425 @default.
• W2300959400 hasConceptScore W2300959400C106804226 @default.
• W2300959400 hasConceptScore W2300959400C109007969 @default.
• W2300959400 hasConceptScore W2300959400C109281948 @default.
• W2300959400 hasConceptScore W2300959400C111368507 @default.
• W2300959400 hasConceptScore W2300959400C112959462 @default.
• W2300959400 hasConceptScore W2300959400C114793014 @default.
• W2300959400 hasConceptScore W2300959400C120806208 @default.
• W2300959400 hasConceptScore W2300959400C122792734 @default.
• W2300959400 hasConceptScore W2300959400C127313418 @default.
• W2300959400 hasConceptScore W2300959400C127491152 @default.
• W2300959400 hasConceptScore W2300959400C151730666 @default.
• W2300959400 hasConceptScore W2300959400C17409809 @default.
• W2300959400 hasConceptScore W2300959400C185933670 @default.
• W2300959400 hasConceptScore W2300959400C18903297 @default.
• W2300959400 hasConceptScore W2300959400C20470049 @default.
• W2300959400 hasConceptScore W2300959400C23389524 @default.
• W2300959400 hasConceptScore W2300959400C2776023875 @default.
• W2300959400 hasConceptScore W2300959400C2776643431 @default.
• W2300959400 hasConceptScore W2300959400C2816523 @default.
• W2300959400 hasConceptScore W2300959400C64297162 @default.
• W2300959400 hasConceptScore W2300959400C6494504 @default.
• W2300959400 hasConceptScore W2300959400C65589250 @default.
• W2300959400 hasConceptScore W2300959400C77928131 @default.
• W2300959400 hasConceptScore W2300959400C86803240 @default.

• next