FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2131454857> ?p ?o ?g. }

• W2131454857 endingPage "263" @default.
• W2131454857 startingPage "249" @default.
• W2131454857 abstract "Carboniferous sedimentation in the southern Gaspé Peninsula has fossilized a paleosurface which is now gradually being exhumed by erosion. Part of the surface was horizontally cut by a major peneplanation event that took place between 290 Ma (Permian) and 200 Ma (Jurassic). Exhumation of the surface below the peneplanation line must also have started by Jurassic time in response to the en bloc uplift of the evolving Atlantic Ocean's passive margins. Some geomorphic features of the exhumed paleosurface bring clues regarding Carboniferous paleoenvironments and tectonics. A planation surface limited by a scarp, which is leading to a higher planation surface occupied by the same rock formations, is here interpreted as a paleo- wave-cut platform (associated to the Windsor transgression) for it cannot be explained by differential erosion, fault movement or etchplanation. A series of fault scarps cutting through planation surfaces are interpreted as being the result of post-Acadian fault activity. The preservation of limestone hogbacks on the exhumed paleosurface, which are interpreted as having evolved under an arid climate, is believed to be either related to a pre-Windsor clastic fossilization or to post-Windsor lateral displacement. The tightly embanked river system, which is still currently dissecting the Peninsula's main planation surface, and the karstic systems of both that surface and the exhumed paleosurface, are interpreted as having evolved since Jurassic Time, except for a few cases of river antecedence in the north-central highlands which are interpreted as representing even older river routes." @default.
• W2131454857 created "2016-06-24" @default.
• W2131454857 creator A5069810931 @default.
• W2131454857 creator A5080416337 @default.
• W2131454857 date "2002-10-02" @default.
• W2131454857 modified "2023-10-18" @default.
• W2131454857 title "Geomorphology of an Exhumed Carboniferous Paleosurface in the Southern Gaspé Peninsula, Québec: Paleoenvironmental and Tectonic Implications" @default.
• W2131454857 cites W1596931549 @default.
• W2131454857 cites W1964776999 @default.
• W2131454857 cites W1965705570 @default.
• W2131454857 cites W1972900894 @default.
• W2131454857 cites W1979699063 @default.
• W2131454857 cites W1979771381 @default.
• W2131454857 cites W1987108099 @default.
• W2131454857 cites W1989407181 @default.
• W2131454857 cites W1991977956 @default.
• W2131454857 cites W1994891433 @default.
• W2131454857 cites W1999149809 @default.
• W2131454857 cites W2016339376 @default.
• W2131454857 cites W2037667328 @default.
• W2131454857 cites W2037825354 @default.
• W2131454857 cites W2062347206 @default.
• W2131454857 cites W2076314924 @default.
• W2131454857 cites W2081296107 @default.
• W2131454857 cites W2089623721 @default.
• W2131454857 cites W2093617398 @default.
• W2131454857 cites W2096298020 @default.
• W2131454857 cites W2108153959 @default.
• W2131454857 cites W2128220143 @default.
• W2131454857 cites W2131483478 @default.
• W2131454857 cites W2143313817 @default.
• W2131454857 cites W2159719088 @default.
• W2131454857 cites W2159877617 @default.
• W2131454857 cites W2313255370 @default.
• W2131454857 cites W2323347294 @default.
• W2131454857 cites W2904029710 @default.
• W2131454857 cites W2908614996 @default.
• W2131454857 cites W2908699175 @default.
• W2131454857 cites W2908821964 @default.
• W2131454857 cites W2909543336 @default.
• W2131454857 cites W2981541066 @default.
• W2131454857 cites W3110858439 @default.
• W2131454857 cites W4212931122 @default.
• W2131454857 cites W4235078485 @default.
• W2131454857 cites W4250950666 @default.
• W2131454857 doi "https://doi.org/10.7202/005690ar" @default.
• W2131454857 hasPublicationYear "2002" @default.
• W2131454857 type Work @default.
• W2131454857 sameAs 2131454857 @default.
• W2131454857 citedByCount "15" @default.
• W2131454857 countsByYear W21314548572013 @default.
• W2131454857 countsByYear W21314548572016 @default.
• W2131454857 countsByYear W21314548572019 @default.
• W2131454857 countsByYear W21314548572021 @default.
• W2131454857 countsByYear W21314548572023 @default.
• W2131454857 crossrefType "journal-article" @default.
• W2131454857 hasAuthorship W2131454857A5069810931 @default.
• W2131454857 hasAuthorship W2131454857A5080416337 @default.
• W2131454857 hasBestOaLocation W21314548571 @default.
• W2131454857 hasConcept C109007969 @default.
• W2131454857 hasConcept C112959462 @default.
• W2131454857 hasConcept C114679195 @default.
• W2131454857 hasConcept C114793014 @default.
• W2131454857 hasConcept C127313418 @default.
• W2131454857 hasConcept C149918038 @default.
• W2131454857 hasConcept C151730666 @default.
• W2131454857 hasConcept C179226041 @default.
• W2131454857 hasConcept C206137718 @default.
• W2131454857 hasConcept C32552466 @default.
• W2131454857 hasConcept C77928131 @default.
• W2131454857 hasConceptScore W2131454857C109007969 @default.
• W2131454857 hasConceptScore W2131454857C112959462 @default.
• W2131454857 hasConceptScore W2131454857C114679195 @default.
• W2131454857 hasConceptScore W2131454857C114793014 @default.
• W2131454857 hasConceptScore W2131454857C127313418 @default.
• W2131454857 hasConceptScore W2131454857C149918038 @default.
• W2131454857 hasConceptScore W2131454857C151730666 @default.
• W2131454857 hasConceptScore W2131454857C179226041 @default.
• W2131454857 hasConceptScore W2131454857C206137718 @default.
• W2131454857 hasConceptScore W2131454857C32552466 @default.
• W2131454857 hasConceptScore W2131454857C77928131 @default.
• W2131454857 hasIssue "2" @default.
• W2131454857 hasLocation W21314548571 @default.
• W2131454857 hasOpenAccess W2131454857 @default.
• W2131454857 hasPrimaryLocation W21314548571 @default.
• W2131454857 hasRelatedWork W1901082281 @default.
• W2131454857 hasRelatedWork W2011551731 @default.
• W2131454857 hasRelatedWork W2028624432 @default.
• W2131454857 hasRelatedWork W2047380333 @default.
• W2131454857 hasRelatedWork W2079528806 @default.
• W2131454857 hasRelatedWork W2584599219 @default.
• W2131454857 hasRelatedWork W3042102297 @default.
• W2131454857 hasRelatedWork W4246619982 @default.
• W2131454857 hasRelatedWork W4378903240 @default.
• W2131454857 hasRelatedWork W4385658230 @default.
• W2131454857 hasVolume "53" @default.
• W2131454857 isParatext "false" @default.
• W2131454857 isRetracted "false" @default.

• next