FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2037553700> ?p ?o ?g. }

• W2037553700 endingPage "202" @default.
• W2037553700 startingPage "181" @default.
• W2037553700 abstract "The creation of accommodation space in subaerial sedimentary environments is closely linked to uplift the source area (along basin–margin faults) or to a rise in base level. Depending (amongst others) on the relative importance of these two factors, the margins of terrestrial sedimentary basins (where alluvial fans develop) produce aggradational, progradational or retrogradational stratigraphic architecture. We studied a total of 43 Quaternary alluvial fans in the Granada and Bajo Segura basins (Betic Cordillera, Spain). The analysis of their stratigraphic architecture and sedimentary facies has revealed the existence of three groups characterised by distinct stratal stacking patterns, which is the result of differences in eustasy and tectonics. The qualitative and quantitative analysis of these alluvial fans and their drainage basins has allowed us to define certain characteristic geomorphological patterns related, in each case, to the main mechanism operative in the creation of accommodation space. These patterns are described as follows. (1) Alluvial aggradation is the main result of high tectonic subsidence with the development of quite open, but small fans with a constant steep slope lacking incised channels and headward-eroding gullies. (2) In contrast, when the principal mechanism in creating accommodation space is low tectonic subsidence, progradation occurs and the fans are narrower and larger. Moreover, the slopes of such fans are less steep in relation to the drainage area than in the above case, being constant or even concave in longitudinal profile. They also have short, deep incised channels, culminating downfan in a depositional lobe. In inactive zones, long, deep headward-eroding gullies develop. (3) Areas of extremely low tectonic subsidence and base level rise produce very open fans in the sedimentary basin, although with a pronounced mountain embayment, which gives them a characteristic “mushroom” shape in plan view. In the latter case, retrogradation is the typical stratigraphic stacking pattern and the fans are quite extensive with respect to their drainage areas, usually showing a segmented longitudinal profile with a low gradient. The feeder channels do not surpass stream order 3, and various extremely long and shallow incised channels can appear. (4) Contrary to the case of fans developing under a regime of subsidence, when the accommodation is due to base level rise, the fan slopes bear no relation to the extent of the catchment basins. In such a case, the overall fan slope is strongly influenced by the extent of the mountain embayment because it determines the distributions of debris and sheet-flows over the alluvial surface." @default.
• W2037553700 created "2016-06-24" @default.
• W2037553700 creator A5016585484 @default.
• W2037553700 creator A5027646920 @default.
• W2037553700 creator A5033042201 @default.
• W2037553700 creator A5044427354 @default.
• W2037553700 date "2003-02-01" @default.
• W2037553700 modified "2023-10-16" @default.
• W2037553700 title "Differential features of alluvial fans controlled by tectonic or eustatic accommodation space. Examples from the Betic Cordillera, Spain" @default.
• W2037553700 cites W1965832912 @default.
• W2037553700 cites W1970208184 @default.
• W2037553700 cites W1982172760 @default.
• W2037553700 cites W1982758111 @default.
• W2037553700 cites W1984281990 @default.
• W2037553700 cites W1987844701 @default.
• W2037553700 cites W1989373718 @default.
• W2037553700 cites W1990436032 @default.
• W2037553700 cites W1991984045 @default.
• W2037553700 cites W1999512919 @default.
• W2037553700 cites W2001682930 @default.
• W2037553700 cites W2010883346 @default.
• W2037553700 cites W2011748659 @default.
• W2037553700 cites W2015717635 @default.
• W2037553700 cites W2023263906 @default.
• W2037553700 cites W2026252880 @default.
• W2037553700 cites W2032130922 @default.
• W2037553700 cites W2033373311 @default.
• W2037553700 cites W2036897912 @default.
• W2037553700 cites W2037559499 @default.
• W2037553700 cites W2039362644 @default.
• W2037553700 cites W2039500268 @default.
• W2037553700 cites W2054688467 @default.
• W2037553700 cites W2064510302 @default.
• W2037553700 cites W2068202401 @default.
• W2037553700 cites W2068517197 @default.
• W2037553700 cites W2074438535 @default.
• W2037553700 cites W2075793015 @default.
• W2037553700 cites W2079239345 @default.
• W2037553700 cites W2086803784 @default.
• W2037553700 cites W2109258353 @default.
• W2037553700 cites W2109942446 @default.
• W2037553700 cites W2112828972 @default.
• W2037553700 cites W2126104633 @default.
• W2037553700 cites W2130994975 @default.
• W2037553700 cites W2134880572 @default.
• W2037553700 cites W2145591683 @default.
• W2037553700 cites W2163718669 @default.
• W2037553700 cites W2330463646 @default.
• W2037553700 cites W3153471564 @default.
• W2037553700 cites W4236383427 @default.
• W2037553700 doi "https://doi.org/10.1016/s0169-555x(02)00214-3" @default.
• W2037553700 hasPublicationYear "2003" @default.
• W2037553700 type Work @default.
• W2037553700 sameAs 2037553700 @default.
• W2037553700 citedByCount "146" @default.
• W2037553700 countsByYear W20375537002012 @default.
• W2037553700 countsByYear W20375537002013 @default.
• W2037553700 countsByYear W20375537002014 @default.
• W2037553700 countsByYear W20375537002015 @default.
• W2037553700 countsByYear W20375537002016 @default.
• W2037553700 countsByYear W20375537002017 @default.
• W2037553700 countsByYear W20375537002018 @default.
• W2037553700 countsByYear W20375537002019 @default.
• W2037553700 countsByYear W20375537002020 @default.
• W2037553700 countsByYear W20375537002021 @default.
• W2037553700 countsByYear W20375537002022 @default.
• W2037553700 countsByYear W20375537002023 @default.
• W2037553700 crossrefType "journal-article" @default.
• W2037553700 hasAuthorship W2037553700A5016585484 @default.
• W2037553700 hasAuthorship W2037553700A5027646920 @default.
• W2037553700 hasAuthorship W2037553700A5033042201 @default.
• W2037553700 hasAuthorship W2037553700A5044427354 @default.
• W2037553700 hasConcept C100951216 @default.
• W2037553700 hasConcept C109007969 @default.
• W2037553700 hasConcept C112959462 @default.
• W2037553700 hasConcept C114793014 @default.
• W2037553700 hasConcept C126753816 @default.
• W2037553700 hasConcept C127313418 @default.
• W2037553700 hasConcept C142614818 @default.
• W2037553700 hasConcept C146588470 @default.
• W2037553700 hasConcept C151730666 @default.
• W2037553700 hasConcept C16565575 @default.
• W2037553700 hasConcept C180851071 @default.
• W2037553700 hasConcept C32552466 @default.
• W2037553700 hasConcept C6494504 @default.
• W2037553700 hasConcept C69823785 @default.
• W2037553700 hasConcept C77928131 @default.
• W2037553700 hasConcept C84983702 @default.
• W2037553700 hasConceptScore W2037553700C100951216 @default.
• W2037553700 hasConceptScore W2037553700C109007969 @default.
• W2037553700 hasConceptScore W2037553700C112959462 @default.
• W2037553700 hasConceptScore W2037553700C114793014 @default.
• W2037553700 hasConceptScore W2037553700C126753816 @default.
• W2037553700 hasConceptScore W2037553700C127313418 @default.
• W2037553700 hasConceptScore W2037553700C142614818 @default.
• W2037553700 hasConceptScore W2037553700C146588470 @default.
• W2037553700 hasConceptScore W2037553700C151730666 @default.
• W2037553700 hasConceptScore W2037553700C16565575 @default.

• next