FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1987923876> ?p ?o ?g. }

• W1987923876 endingPage "1753" @default.
• W1987923876 startingPage "1739" @default.
• W1987923876 abstract "The ancient Laurentian margin rifted in the latest Neoproterozoic to early Cambrian but appears not to have developed as a simple passive margin through a long, post-rift, drift phase. Stratigraphic and conodont biostratigraphic information from four platform-to-basin transects across the margin has advanced our knowledge of the early Paleozoic evolution of the margin. In northeastern British Columbia, two northern transects span the Macdonald Platform to Kechika Trough and Ospika Embayment, and a third transect spans the parautochthonous Cassiar Terrane. In the southern Rocky Mountains, new conodont biostratigraphic data for the Ordovician succession of the Bow Platform is correlated to coeval basinal facies of the White River Trough. In total, from 26 stratigraphic sections, over 25 km of strata were measured and > 1200 conodont samples were collected that yielded over 100 000 conodont elements. Key zonal species were used for regional correlation of uppermost Cambrian to Middle Devonian strata along the Cordillera. The biostratigraphy temporally constrains at least two periods of renewed extension along the margin, in the latest Cambrian and late Early Ordovician. Alkalic volcanics associated with abrupt facies changes across the ancient shelf break, intervals of slope debris breccia deposits, and distal turbidite flows suggest the margin was characterized by intervals of volcanism, basin foundering, and platform flooding. Siliciclastics in the succession were sourced by a reactivation of tectonic highs, such as the Peace River Arch. Prominent hiatuses punctuate the succession, including unconformities of early Late Ordovician, sub-Llandovery, possibly Early to Middle Silurian and Early Devonian ages." @default.
• W1987923876 created "2016-06-24" @default.
• W1987923876 creator A5016837717 @default.
• W1987923876 creator A5087467341 @default.
• W1987923876 date "2003-12-01" @default.
• W1987923876 modified "2023-10-18" @default.
• W1987923876 title "Lower Paleozoic stratigraphic and biostratigraphic correlations in the Canadian Cordillera: implications for the tectonic evolution of the Laurentian margin" @default.
• W1987923876 cites W1963566708 @default.
• W1987923876 cites W1967824957 @default.
• W1987923876 cites W1973232630 @default.
• W1987923876 cites W1979412245 @default.
• W1987923876 cites W1980372107 @default.
• W1987923876 cites W1981677666 @default.
• W1987923876 cites W1986350531 @default.
• W1987923876 cites W1990058169 @default.
• W1987923876 cites W1990953788 @default.
• W1987923876 cites W1994917745 @default.
• W1987923876 cites W2008519747 @default.
• W1987923876 cites W2070222686 @default.
• W1987923876 cites W2076615234 @default.
• W1987923876 cites W2078308820 @default.
• W1987923876 cites W2078553842 @default.
• W1987923876 cites W2087208845 @default.
• W1987923876 cites W2097018988 @default.
• W1987923876 cites W2097646890 @default.
• W1987923876 cites W2099035295 @default.
• W1987923876 cites W2116699008 @default.
• W1987923876 cites W2123117885 @default.
• W1987923876 cites W2143470322 @default.
• W1987923876 cites W2160341775 @default.
• W1987923876 cites W2160427602 @default.
• W1987923876 cites W2260335191 @default.
• W1987923876 cites W2268262318 @default.
• W1987923876 cites W2607297173 @default.
• W1987923876 cites W2644132672 @default.
• W1987923876 cites W2974295936 @default.
• W1987923876 cites W4243082928 @default.
• W1987923876 doi "https://doi.org/10.1139/e03-049" @default.
• W1987923876 hasPublicationYear "2003" @default.
• W1987923876 type Work @default.
• W1987923876 sameAs 1987923876 @default.
• W1987923876 citedByCount "23" @default.
• W1987923876 countsByYear W19879238762012 @default.
• W1987923876 countsByYear W19879238762013 @default.
• W1987923876 countsByYear W19879238762014 @default.
• W1987923876 countsByYear W19879238762015 @default.
• W1987923876 countsByYear W19879238762016 @default.
• W1987923876 countsByYear W19879238762017 @default.
• W1987923876 countsByYear W19879238762019 @default.
• W1987923876 countsByYear W19879238762020 @default.
• W1987923876 countsByYear W19879238762023 @default.
• W1987923876 crossrefType "journal-article" @default.
• W1987923876 hasAuthorship W1987923876A5016837717 @default.
• W1987923876 hasAuthorship W1987923876A5087467341 @default.
• W1987923876 hasConcept C107832698 @default.
• W1987923876 hasConcept C109007969 @default.
• W1987923876 hasConcept C127313418 @default.
• W1987923876 hasConcept C13106087 @default.
• W1987923876 hasConcept C139719470 @default.
• W1987923876 hasConcept C146588470 @default.
• W1987923876 hasConcept C149918038 @default.
• W1987923876 hasConcept C151730666 @default.
• W1987923876 hasConcept C162324750 @default.
• W1987923876 hasConcept C181727316 @default.
• W1987923876 hasConcept C191735495 @default.
• W1987923876 hasConcept C201633675 @default.
• W1987923876 hasConcept C2779004622 @default.
• W1987923876 hasConcept C2781148125 @default.
• W1987923876 hasConcept C32239851 @default.
• W1987923876 hasConcept C50682988 @default.
• W1987923876 hasConcept C61721801 @default.
• W1987923876 hasConcept C77928131 @default.
• W1987923876 hasConcept C91442348 @default.
• W1987923876 hasConceptScore W1987923876C107832698 @default.
• W1987923876 hasConceptScore W1987923876C109007969 @default.
• W1987923876 hasConceptScore W1987923876C127313418 @default.
• W1987923876 hasConceptScore W1987923876C13106087 @default.
• W1987923876 hasConceptScore W1987923876C139719470 @default.
• W1987923876 hasConceptScore W1987923876C146588470 @default.
• W1987923876 hasConceptScore W1987923876C149918038 @default.
• W1987923876 hasConceptScore W1987923876C151730666 @default.
• W1987923876 hasConceptScore W1987923876C162324750 @default.
• W1987923876 hasConceptScore W1987923876C181727316 @default.
• W1987923876 hasConceptScore W1987923876C191735495 @default.
• W1987923876 hasConceptScore W1987923876C201633675 @default.
• W1987923876 hasConceptScore W1987923876C2779004622 @default.
• W1987923876 hasConceptScore W1987923876C2781148125 @default.
• W1987923876 hasConceptScore W1987923876C32239851 @default.
• W1987923876 hasConceptScore W1987923876C50682988 @default.
• W1987923876 hasConceptScore W1987923876C61721801 @default.
• W1987923876 hasConceptScore W1987923876C77928131 @default.
• W1987923876 hasConceptScore W1987923876C91442348 @default.
• W1987923876 hasIssue "12" @default.
• W1987923876 hasLocation W19879238761 @default.
• W1987923876 hasOpenAccess W1987923876 @default.
• W1987923876 hasPrimaryLocation W19879238761 @default.
• W1987923876 hasRelatedWork W1987923876 @default.
• W1987923876 hasRelatedWork W2056293580 @default.

• next