Matches in SemOpenAlex for { <https://semopenalex.org/work/W2146702900> ?p ?o ?g. }
Showing items 1 to 91 of
91
with 100 items per page.
- W2146702900 endingPage "603" @default.
- W2146702900 startingPage "587" @default.
- W2146702900 abstract "The magnitude and timing of synorogenic and postorogenic denudation along fold and thrust belts and their associated foreland basins, of interest because of both tectonic and economic implications, is generally poorly constrained. Along the late Paleozoic Ouachita trend, a thin veneer of Cretaceous strata is preserved above a low-relief erosional surface that beveled the Ouachita orogen and adjacent foreland areas. This regional erosion surface provides a valuable constraint for interpreting new and previously published apatite fission track (AFT) data obtained from exposed structural highs along the Ouachita trend (Marathon, Llano, Arbuckle, and Benton uplifts). AFT data from sampled localities within the deformation belt (Marathon and Benton uplifts) exhibit younger ages and, generally, longer mean lengths than data from localities on the foreland side of the deformation front (Llano and Arbuckle uplifts). This observation suggests that erosion of the orogen, rather than its extensional collapse, was the primary mechanism responsible for flexural isostatic unloading of the foreland crust. In addition, all samples show evidence for mild reheating following their pre-Cretaceous cooling history. Specifically, the lack of a significant population of >14.5-μm tracks in all samples appears to require residence at temperatures of ≥55°±5°C after development of the sub-Cretaceous erosional surface. This implies that ∼1000 m of Cretaceous-Paleogene (?) strata were deposited across the entire Ouachita frontal trend and subsequently removed during later Tertiary time. This Tertiary denudation is interpreted to reflect the interplay between regional denudation and isostatic compensation in response to slow (∼10 m/m.y.) epeirogenic uplift of the southern midcontinent and a long-term drop (∼200 m) in eustatic sealevel during this time." @default.
- W2146702900 created "2016-06-24" @default.
- W2146702900 creator A5037353021 @default.
- W2146702900 creator A5044902887 @default.
- W2146702900 creator A5088065883 @default.
- W2146702900 creator A5091837937 @default.
- W2146702900 date "1998-08-01" @default.
- W2146702900 modified "2023-10-17" @default.
- W2146702900 title "Postorogenic denudation along the late Paleozoic Ouachita trend, south central United States of America: Magnitude and timing constraints from apatite fission track data" @default.
- W2146702900 cites W146939729 @default.
- W2146702900 cites W1791776832 @default.
- W2146702900 cites W1967643354 @default.
- W2146702900 cites W1979654629 @default.
- W2146702900 cites W1987005841 @default.
- W2146702900 cites W1987738609 @default.
- W2146702900 cites W1997252211 @default.
- W2146702900 cites W2007596578 @default.
- W2146702900 cites W2012373503 @default.
- W2146702900 cites W2022656685 @default.
- W2146702900 cites W2023013057 @default.
- W2146702900 cites W2033216734 @default.
- W2146702900 cites W2060504234 @default.
- W2146702900 cites W2077309788 @default.
- W2146702900 cites W2086264308 @default.
- W2146702900 cites W2091414028 @default.
- W2146702900 cites W2092088247 @default.
- W2146702900 cites W2105948858 @default.
- W2146702900 cites W2128004689 @default.
- W2146702900 cites W2133737681 @default.
- W2146702900 cites W2149693612 @default.
- W2146702900 cites W2161689334 @default.
- W2146702900 cites W2488817644 @default.
- W2146702900 cites W4229829874 @default.
- W2146702900 cites W4243424366 @default.
- W2146702900 doi "https://doi.org/10.1029/98tc01316" @default.
- W2146702900 hasPublicationYear "1998" @default.
- W2146702900 type Work @default.
- W2146702900 sameAs 2146702900 @default.
- W2146702900 citedByCount "24" @default.
- W2146702900 countsByYear W21467029002012 @default.
- W2146702900 countsByYear W21467029002014 @default.
- W2146702900 countsByYear W21467029002015 @default.
- W2146702900 countsByYear W21467029002016 @default.
- W2146702900 countsByYear W21467029002018 @default.
- W2146702900 countsByYear W21467029002019 @default.
- W2146702900 countsByYear W21467029002022 @default.
- W2146702900 crossrefType "journal-article" @default.
- W2146702900 hasAuthorship W2146702900A5037353021 @default.
- W2146702900 hasAuthorship W2146702900A5044902887 @default.
- W2146702900 hasAuthorship W2146702900A5088065883 @default.
- W2146702900 hasAuthorship W2146702900A5091837937 @default.
- W2146702900 hasBestOaLocation W21467029001 @default.
- W2146702900 hasConcept C114793014 @default.
- W2146702900 hasConcept C12294951 @default.
- W2146702900 hasConcept C127313418 @default.
- W2146702900 hasConcept C151730666 @default.
- W2146702900 hasConcept C193748577 @default.
- W2146702900 hasConcept C2777241186 @default.
- W2146702900 hasConcept C77928131 @default.
- W2146702900 hasConcept C87432785 @default.
- W2146702900 hasConcept C92217149 @default.
- W2146702900 hasConceptScore W2146702900C114793014 @default.
- W2146702900 hasConceptScore W2146702900C12294951 @default.
- W2146702900 hasConceptScore W2146702900C127313418 @default.
- W2146702900 hasConceptScore W2146702900C151730666 @default.
- W2146702900 hasConceptScore W2146702900C193748577 @default.
- W2146702900 hasConceptScore W2146702900C2777241186 @default.
- W2146702900 hasConceptScore W2146702900C77928131 @default.
- W2146702900 hasConceptScore W2146702900C87432785 @default.
- W2146702900 hasConceptScore W2146702900C92217149 @default.
- W2146702900 hasIssue "4" @default.
- W2146702900 hasLocation W21467029001 @default.
- W2146702900 hasOpenAccess W2146702900 @default.
- W2146702900 hasPrimaryLocation W21467029001 @default.
- W2146702900 hasRelatedWork W2019716342 @default.
- W2146702900 hasRelatedWork W2035407149 @default.
- W2146702900 hasRelatedWork W2146702900 @default.
- W2146702900 hasRelatedWork W2160812439 @default.
- W2146702900 hasRelatedWork W2336786207 @default.
- W2146702900 hasRelatedWork W2375464054 @default.
- W2146702900 hasRelatedWork W2379607764 @default.
- W2146702900 hasRelatedWork W3202265117 @default.
- W2146702900 hasRelatedWork W4289755559 @default.
- W2146702900 hasRelatedWork W2099330809 @default.
- W2146702900 hasVolume "17" @default.
- W2146702900 isParatext "false" @default.
- W2146702900 isRetracted "false" @default.
- W2146702900 magId "2146702900" @default.
- W2146702900 workType "article" @default.