FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3045643879> ?p ?o ?g. }

• W3045643879 endingPage "477" @default.
• W3045643879 startingPage "450" @default.
• W3045643879 abstract "The thrust front of the Northern Appalachians involves Ediacaran rift-related structures of the Laurentian margin that were re-worked in Taconic (Ordovician), Salinic (mainly Silurian) and Acadian (mainly Devonian) deformation events. Much of the thrust front is concealed under the Gulf of St. Lawrence, but Port au Port Peninsula, in western Newfoundland provides a cross-section through the Laurentian passive margin, overlying foreland basins, and the Humber Arm Allochthon. A large area of foreland basin strata is present in areas formerly mapped as Humber Arm Allochthon. Abrupt thickness changes and an abundance of fault-scarp-derived limestone conglomerate indicate that deposition was influenced by block faulting and differential subsidence in a basin undergoing active flexural extension. A coarsening upward trend in the Goose Tickle Group represents a transition from a distal to a proximal sediment source as the Humber Arm Allochthon was emplaced westwards. Goose Tickle Group separates two packages of allochthonous rocks. The West Bay Thrust Sheet, the lower package, represents the leading edge of the Taconic allochthon. Its timing of emplacement is constrained by Darriwilian 3 graptolites both above and below the thrust sheet. Its present-day configuration results from a combination of processes including thrusting, extension by gravity spreading, gravity gliding, and subsequent erosion of material that was deposited in the Goose Tickle Group. The structurally higher Lourdes Thrust Sheet is an out-of-sequence structure associated with Acadian (Devonian) orogenesis. High-angle faults show a protracted history of movement that includes early Taconic flexural extension, Acadian inversion, and later Carboniferous or Mesozoic strike-slip motion. The leading edge of the Humber Arm Allochthon was influenced by both thin-skinned and thick-skinned tectonics throughout the development of the Appalachian orogen." @default.
• W3045643879 created "2020-08-03" @default.
• W3045643879 creator A5038078094 @default.
• W3045643879 creator A5075166418 @default.
• W3045643879 creator A5075716377 @default.
• W3045643879 date "2020-05-01" @default.
• W3045643879 modified "2023-09-25" @default.
• W3045643879 title "Tectonics and foreland basin development at the leading edge of the Humber Arm Allochthon, western Newfoundland, Canadian Appalachians" @default.
• W3045643879 cites W131384788 @default.
• W3045643879 cites W1534952052 @default.
• W3045643879 cites W1540907293 @default.
• W3045643879 cites W1776479751 @default.
• W3045643879 cites W1842536088 @default.
• W3045643879 cites W1858701478 @default.
• W3045643879 cites W1881605923 @default.
• W3045643879 cites W1969172353 @default.
• W3045643879 cites W1969961393 @default.
• W3045643879 cites W1973170581 @default.
• W3045643879 cites W1977151267 @default.
• W3045643879 cites W1980693547 @default.
• W3045643879 cites W1981828811 @default.
• W3045643879 cites W1985039445 @default.
• W3045643879 cites W1986092739 @default.
• W3045643879 cites W1992106748 @default.
• W3045643879 cites W1992871671 @default.
• W3045643879 cites W1995504700 @default.
• W3045643879 cites W2000400065 @default.
• W3045643879 cites W2011893217 @default.
• W3045643879 cites W2015322020 @default.
• W3045643879 cites W2019461920 @default.
• W3045643879 cites W2024077172 @default.
• W3045643879 cites W2024280738 @default.
• W3045643879 cites W2039320884 @default.
• W3045643879 cites W2062090437 @default.
• W3045643879 cites W2065168337 @default.
• W3045643879 cites W2071129416 @default.
• W3045643879 cites W2073718887 @default.
• W3045643879 cites W2075929381 @default.
• W3045643879 cites W2087869071 @default.
• W3045643879 cites W2090599254 @default.
• W3045643879 cites W2091539779 @default.
• W3045643879 cites W2094124295 @default.
• W3045643879 cites W2113253074 @default.
• W3045643879 cites W2117052568 @default.
• W3045643879 cites W2132661912 @default.
• W3045643879 cites W2141384256 @default.
• W3045643879 cites W2143128079 @default.
• W3045643879 cites W2150854303 @default.
• W3045643879 cites W2151823860 @default.
• W3045643879 cites W2158242164 @default.
• W3045643879 cites W2183556358 @default.
• W3045643879 cites W2325642434 @default.
• W3045643879 cites W2502971937 @default.
• W3045643879 cites W2521129314 @default.
• W3045643879 cites W2628269717 @default.
• W3045643879 cites W2807630476 @default.
• W3045643879 cites W2910165085 @default.
• W3045643879 cites W2910673852 @default.
• W3045643879 cites W2922153851 @default.
• W3045643879 cites W2929117452 @default.
• W3045643879 cites W302196161 @default.
• W3045643879 cites W3123277409 @default.
• W3045643879 cites W615529848 @default.
• W3045643879 cites W82534810 @default.
• W3045643879 doi "https://doi.org/10.2475/05.2020.02" @default.
• W3045643879 hasPublicationYear "2020" @default.
• W3045643879 type Work @default.
• W3045643879 sameAs 3045643879 @default.
• W3045643879 citedByCount "4" @default.
• W3045643879 countsByYear W30456438792021 @default.
• W3045643879 countsByYear W30456438792022 @default.
• W3045643879 countsByYear W30456438792023 @default.
• W3045643879 crossrefType "journal-article" @default.
• W3045643879 hasAuthorship W3045643879A5038078094 @default.
• W3045643879 hasAuthorship W3045643879A5075166418 @default.
• W3045643879 hasAuthorship W3045643879A5075716377 @default.
• W3045643879 hasConcept C107832698 @default.
• W3045643879 hasConcept C109007969 @default.
• W3045643879 hasConcept C110041135 @default.
• W3045643879 hasConcept C114679195 @default.
• W3045643879 hasConcept C114793014 @default.
• W3045643879 hasConcept C127313418 @default.
• W3045643879 hasConcept C151730666 @default.
• W3045643879 hasConcept C153220577 @default.
• W3045643879 hasConcept C165205528 @default.
• W3045643879 hasConcept C175551986 @default.
• W3045643879 hasConcept C193748577 @default.
• W3045643879 hasConcept C2776520773 @default.
• W3045643879 hasConcept C2780802278 @default.
• W3045643879 hasConcept C50682988 @default.
• W3045643879 hasConcept C77928131 @default.
• W3045643879 hasConcept C91442348 @default.
• W3045643879 hasConceptScore W3045643879C107832698 @default.
• W3045643879 hasConceptScore W3045643879C109007969 @default.
• W3045643879 hasConceptScore W3045643879C110041135 @default.
• W3045643879 hasConceptScore W3045643879C114679195 @default.
• W3045643879 hasConceptScore W3045643879C114793014 @default.
• W3045643879 hasConceptScore W3045643879C127313418 @default.

• next