FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022860556> ?p ?o ?g. }

• W2022860556 endingPage "41" @default.
• W2022860556 startingPage "22" @default.
• W2022860556 abstract "This paper re-examines the Upper Miocene Upper Mount Messenger Formation, Taranaki Basin, to characterize its architecture and interpret its environmental evolution. Analysis of stratal architecture, lithofacies distributions, and paleotransport directions over the 250 m thick formation shows the outcrops provide a nearly dip parallel section displaying the lateral relationships between contemporaneous channel-levee and overbank depositional environments. At least five 30–40 m thick upward fining units are recognized in the north-central parts of the outcrop and are interpreted as large-scale overbank avulsion cycles. Each unit consists of thick- to medium-bedded predominantly planar laminated sandstone turbidites at the base that fine upward into thin- to very thin-bedded, planar laminated and ripple cross-laminated mud-rich turbidites. The units are traceable laterally over a distance exceeding 3 km where they are cut by channels that show basal mudstone draped by medium- to thin-bedded sandstone, and onlapped by thick-bedded planar laminated sandstone at the margin. The channels are separated by tapered packages of medium- to thin-bedded turbidites containing climbing-ripple cross-lamination interpreted as levees. The individual channel-levee and overbank avulsion cycles formed through four stages: 1) a channel avulsion spread sand into the overbank as an unconfined splay, 2) preferential scouring in one area of the splay led to development of a channel with small levees that prograded across the splay, 3) a deep incision followed by abandonment of the channel deposited a mud lining. Alternatively, the mud lining was formed during the first stage as the downdip portion of the channel was abandoned. 4) The channel filled at first by thick-bedded planar laminated and then by climbing-ripple cross-laminated sand. At this time, the growth of constructional levees progressively limited sand into the overbank. Ratios of Bouma division thicknesses calculated over a stratigraphic interval present a new method to distinguish deep-water depositional environments." @default.
• W2022860556 created "2016-06-24" @default.
• W2022860556 creator A5019581661 @default.
• W2022860556 creator A5063961064 @default.
• W2022860556 creator A5072532003 @default.
• W2022860556 creator A5068574227 @default.
• W2022860556 date "2014-04-01" @default.
• W2022860556 modified "2023-09-27" @default.
• W2022860556 title "Stratigraphic architecture and evolution of a deep-water slope channel-levee and overbank apron: The Upper Miocene Upper Mount Messenger Formation, Taranaki Basin" @default.
• W2022860556 cites W1483157968 @default.
• W2022860556 cites W1760845080 @default.
• W2022860556 cites W1875603546 @default.
• W2022860556 cites W1908834558 @default.
• W2022860556 cites W1963700332 @default.
• W2022860556 cites W1969654491 @default.
• W2022860556 cites W1972201367 @default.
• W2022860556 cites W1992872822 @default.
• W2022860556 cites W2006069478 @default.
• W2022860556 cites W2012180822 @default.
• W2022860556 cites W2027123470 @default.
• W2022860556 cites W2039478111 @default.
• W2022860556 cites W2044567705 @default.
• W2022860556 cites W2051298394 @default.
• W2022860556 cites W2055705198 @default.
• W2022860556 cites W2058366022 @default.
• W2022860556 cites W2068377164 @default.
• W2022860556 cites W2074953445 @default.
• W2022860556 cites W2077021680 @default.
• W2022860556 cites W2084064600 @default.
• W2022860556 cites W2089207774 @default.
• W2022860556 cites W2091719389 @default.
• W2022860556 cites W2103006247 @default.
• W2022860556 cites W2106050176 @default.
• W2022860556 cites W2106161981 @default.
• W2022860556 cites W2107226665 @default.
• W2022860556 cites W2109889853 @default.
• W2022860556 cites W2109989023 @default.
• W2022860556 cites W2110082690 @default.
• W2022860556 cites W2113384747 @default.
• W2022860556 cites W2130025140 @default.
• W2022860556 cites W2132524309 @default.
• W2022860556 cites W2148633275 @default.
• W2022860556 cites W2160113537 @default.
• W2022860556 cites W2170678163 @default.
• W2022860556 cites W2322694238 @default.
• W2022860556 cites W2489691169 @default.
• W2022860556 cites W2726630601 @default.
• W2022860556 doi "https://doi.org/10.1016/j.marpetgeo.2014.01.006" @default.
• W2022860556 hasPublicationYear "2014" @default.
• W2022860556 type Work @default.
• W2022860556 sameAs 2022860556 @default.
• W2022860556 citedByCount "21" @default.
• W2022860556 countsByYear W20228605562014 @default.
• W2022860556 countsByYear W20228605562015 @default.
• W2022860556 countsByYear W20228605562016 @default.
• W2022860556 countsByYear W20228605562018 @default.
• W2022860556 countsByYear W20228605562019 @default.
• W2022860556 countsByYear W20228605562020 @default.
• W2022860556 countsByYear W20228605562021 @default.
• W2022860556 countsByYear W20228605562022 @default.
• W2022860556 countsByYear W20228605562023 @default.
• W2022860556 crossrefType "journal-article" @default.
• W2022860556 hasAuthorship W2022860556A5019581661 @default.
• W2022860556 hasAuthorship W2022860556A5063961064 @default.
• W2022860556 hasAuthorship W2022860556A5068574227 @default.
• W2022860556 hasAuthorship W2022860556A5072532003 @default.
• W2022860556 hasConcept C109007969 @default.
• W2022860556 hasConcept C114793014 @default.
• W2022860556 hasConcept C115038398 @default.
• W2022860556 hasConcept C126753816 @default.
• W2022860556 hasConcept C127313418 @default.
• W2022860556 hasConcept C134872888 @default.
• W2022860556 hasConcept C146588470 @default.
• W2022860556 hasConcept C147690470 @default.
• W2022860556 hasConcept C151730666 @default.
• W2022860556 hasConcept C169212394 @default.
• W2022860556 hasConcept C187320778 @default.
• W2022860556 hasConcept C5900021 @default.
• W2022860556 hasConcept C70004062 @default.
• W2022860556 hasConceptScore W2022860556C109007969 @default.
• W2022860556 hasConceptScore W2022860556C114793014 @default.
• W2022860556 hasConceptScore W2022860556C115038398 @default.
• W2022860556 hasConceptScore W2022860556C126753816 @default.
• W2022860556 hasConceptScore W2022860556C127313418 @default.
• W2022860556 hasConceptScore W2022860556C134872888 @default.
• W2022860556 hasConceptScore W2022860556C146588470 @default.
• W2022860556 hasConceptScore W2022860556C147690470 @default.
• W2022860556 hasConceptScore W2022860556C151730666 @default.
• W2022860556 hasConceptScore W2022860556C169212394 @default.
• W2022860556 hasConceptScore W2022860556C187320778 @default.
• W2022860556 hasConceptScore W2022860556C5900021 @default.
• W2022860556 hasConceptScore W2022860556C70004062 @default.
• W2022860556 hasLocation W20228605561 @default.
• W2022860556 hasOpenAccess W2022860556 @default.
• W2022860556 hasPrimaryLocation W20228605561 @default.
• W2022860556 hasRelatedWork W1518698663 @default.
• W2022860556 hasRelatedWork W2077902624 @default.
• W2022860556 hasRelatedWork W2101072177 @default.

• next