FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2158492007> ?p ?o ?g. }

• W2158492007 endingPage "236" @default.
• W2158492007 startingPage "207" @default.
• W2158492007 abstract "Drilling offshore from Cape Roberts, Antarctica, has enabled recovery of a 1472-m cumulative record of late Eocene–early Miocene history of sedimentary basin development and climate change in the Western Ross Sea. In this paper, we synthesize the results of palaeomagnetic analyses carried out on the CRP-1, CRP-2 and CRP-3 sediment cores, and present a chronology for the recovered Eocene–Miocene succession. Stepwise demagnetization data demonstrate that secondary overprints have been successfully removed and that characteristic remanent magnetizations (ChRMs) have been clearly identified in most of the samples. A close sampling interval has allowed a detailed magnetic polarity stratigraphy to be established for the composite succession. Correlation with the geomagnetic polarity time scale (GPTS) has been constrained by a number of 40Ar/39Ar and 87Sr/86Sr ages, as well as by a recently developed Antarctic siliceous microfossil zonation, and by calcareous nannoplankton biostratigraphy. The basal sediments of the Eocene–Miocene succession rest unconformably on Devonian sandstones of the Beacon Supergroup. A basal sandstone breccia, which probably represents the onset of rifting in the Victoria Land Basin (VLB), is overlain by a succession of sandstones that are interbedded with thin conglomerate beds. These sediments give way to more clearly glacially influenced mudstones and diamictite facies in the mid Oligocene, and, by the Oligocene–Miocene boundary, coincident with the Mi-1 glaciation, a permanent glacial dominance was imprinted on the sedimentary record. Average sediment accumulation rates were initially rapid in the late Eocene–early Oligocene (up to 60 cm/k.y.), but reduced to only a few cm/k.y. in the early Miocene as basin subsidence slowed." @default.
• W2158492007 created "2016-06-24" @default.
• W2158492007 creator A5000659266 @default.
• W2158492007 creator A5003059829 @default.
• W2158492007 creator A5007258078 @default.
• W2158492007 creator A5037172696 @default.
• W2158492007 creator A5077436812 @default.
• W2158492007 date "2005-02-01" @default.
• W2158492007 modified "2023-10-18" @default.
• W2158492007 title "Magnetostratigraphic chronology of a late Eocene to early Miocene glacimarine succession from the Victoria Land Basin, Ross Sea, Antarctica" @default.
• W2158492007 cites W1823431629 @default.
• W2158492007 cites W1973131361 @default.
• W2158492007 cites W2005969926 @default.
• W2158492007 cites W2015522331 @default.
• W2158492007 cites W2015587215 @default.
• W2158492007 cites W2029212877 @default.
• W2158492007 cites W2041883260 @default.
• W2158492007 cites W2043216599 @default.
• W2158492007 cites W2044612552 @default.
• W2158492007 cites W2045213442 @default.
• W2158492007 cites W2052128667 @default.
• W2158492007 cites W2054410655 @default.
• W2158492007 cites W2055215237 @default.
• W2158492007 cites W2058359525 @default.
• W2158492007 cites W2063404386 @default.
• W2158492007 cites W2064821698 @default.
• W2158492007 cites W2066184221 @default.
• W2158492007 cites W2068615100 @default.
• W2158492007 cites W2076505736 @default.
• W2158492007 cites W2096557357 @default.
• W2158492007 cites W2108316127 @default.
• W2158492007 cites W2115575384 @default.
• W2158492007 cites W2118204502 @default.
• W2158492007 cites W2138800991 @default.
• W2158492007 cites W2154082181 @default.
• W2158492007 cites W2154996984 @default.
• W2158492007 cites W2163794040 @default.
• W2158492007 doi "https://doi.org/10.1016/j.gloplacha.2004.09.009" @default.
• W2158492007 hasPublicationYear "2005" @default.
• W2158492007 type Work @default.
• W2158492007 sameAs 2158492007 @default.
• W2158492007 citedByCount "55" @default.
• W2158492007 countsByYear W21584920072012 @default.
• W2158492007 countsByYear W21584920072013 @default.
• W2158492007 countsByYear W21584920072014 @default.
• W2158492007 countsByYear W21584920072015 @default.
• W2158492007 countsByYear W21584920072016 @default.
• W2158492007 countsByYear W21584920072017 @default.
• W2158492007 countsByYear W21584920072018 @default.
• W2158492007 countsByYear W21584920072019 @default.
• W2158492007 countsByYear W21584920072020 @default.
• W2158492007 countsByYear W21584920072021 @default.
• W2158492007 countsByYear W21584920072022 @default.
• W2158492007 crossrefType "journal-article" @default.
• W2158492007 hasAuthorship W2158492007A5000659266 @default.
• W2158492007 hasAuthorship W2158492007A5003059829 @default.
• W2158492007 hasAuthorship W2158492007A5007258078 @default.
• W2158492007 hasAuthorship W2158492007A5037172696 @default.
• W2158492007 hasAuthorship W2158492007A5077436812 @default.
• W2158492007 hasConcept C106804226 @default.
• W2158492007 hasConcept C109007969 @default.
• W2158492007 hasConcept C127313418 @default.
• W2158492007 hasConcept C146588470 @default.
• W2158492007 hasConcept C151730666 @default.
• W2158492007 hasConcept C15739521 @default.
• W2158492007 hasConcept C189479680 @default.
• W2158492007 hasConcept C2778648423 @default.
• W2158492007 hasConcept C2779421809 @default.
• W2158492007 hasConcept C49015763 @default.
• W2158492007 hasConcept C61721801 @default.
• W2158492007 hasConcept C6494504 @default.
• W2158492007 hasConceptScore W2158492007C106804226 @default.
• W2158492007 hasConceptScore W2158492007C109007969 @default.
• W2158492007 hasConceptScore W2158492007C127313418 @default.
• W2158492007 hasConceptScore W2158492007C146588470 @default.
• W2158492007 hasConceptScore W2158492007C151730666 @default.
• W2158492007 hasConceptScore W2158492007C15739521 @default.
• W2158492007 hasConceptScore W2158492007C189479680 @default.
• W2158492007 hasConceptScore W2158492007C2778648423 @default.
• W2158492007 hasConceptScore W2158492007C2779421809 @default.
• W2158492007 hasConceptScore W2158492007C49015763 @default.
• W2158492007 hasConceptScore W2158492007C61721801 @default.
• W2158492007 hasConceptScore W2158492007C6494504 @default.
• W2158492007 hasIssue "1-3" @default.
• W2158492007 hasLocation W21584920071 @default.
• W2158492007 hasOpenAccess W2158492007 @default.
• W2158492007 hasPrimaryLocation W21584920071 @default.
• W2158492007 hasRelatedWork W1565528355 @default.
• W2158492007 hasRelatedWork W2004884347 @default.
• W2158492007 hasRelatedWork W2012310214 @default.
• W2158492007 hasRelatedWork W2059948987 @default.
• W2158492007 hasRelatedWork W2102177510 @default.
• W2158492007 hasRelatedWork W2161176322 @default.
• W2158492007 hasRelatedWork W2355486609 @default.
• W2158492007 hasRelatedWork W2595561582 @default.
• W2158492007 hasRelatedWork W4236804995 @default.
• W2158492007 hasRelatedWork W910486582 @default.
• W2158492007 hasVolume "45" @default.

• next