FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2017640044> ?p ?o ?g. }

• W2017640044 endingPage "377" @default.
• W2017640044 startingPage "363" @default.
• W2017640044 abstract "To better understand the sedimentary history of the erosional crater of Makhtesh Hazera in the hyper-arid Negev Desert of southern Israel we have measured concentrations of in situ 10Be in alluvial sediments from the active drainage system and from abandoned alluvial terraces and dated them using optically stimulated luminescence (OSL). These sedimentary sequences suggest changes in the drainage system behavior over time and show a periodic pattern in which periods of sediment aggradation alternate with periods of degradation through incision and erosion. In alluvial terrace sediments, 10Be concentrations were combined with OSL ages to gain insight of the temporal framework of sediment deposition and shed light on the process of sediment storage. OSL and simple 10Be exposure ages of terrace sediments give deposition ages between ~ 340 ka to ~ 50 ka, at which time the youngest alluvial terrace was incised. Deposition was interrupted twice, at ~ 300 ka and ~ 160 ka, when periods of rapid incision caused the abandonment of the active fluvial surface and the stabilization of a younger and lower fluvial surface. In the active drainage system, 10Be concentrations suggest several possible quartz sources, of which the Lower Cretaceous sandstone bedrock exposed at the base of the cliff enclosing the Makhtesh is the most dominant. The results suggest that sediment eroding form these cliffs are conveyed through the active alluvial channels without significant sediment contribution from alluvial terraces or from eroded bedrock exposed within the Makhtesh. In contrast to our measurements in the active drainage system, 10Be concentrations in alluvial terrace sediments record significant storage within the Makhtesh. We suggest that the geometry of the Makhtesh, mainly the disproportion between the size of the Makhtesh and its narrow outlet, leads to significant accumulation of sediment within the Makhtesh. Episodic breaching of the barrier is followed by rapid and short-lived incision into the stored sediment. The long residence time of sediment within the Makhtesh results in high measured 10Be concentrations. At the end of each of these short incision episodes, when channels are already carved into the alluvial sediment and terraces are formed, the channels only convey sediment directly eroded from the bounding cliff of the Makhtesh; a situation presently observed." @default.
• W2017640044 created "2016-06-24" @default.
• W2017640044 creator A5006721636 @default.
• W2017640044 creator A5014110342 @default.
• W2017640044 creator A5059267263 @default.
• W2017640044 creator A5087720865 @default.
• W2017640044 date "2011-11-01" @default.
• W2017640044 modified "2023-10-06" @default.
• W2017640044 title "Revealing sediment sources, mixing, and transport during erosional crater evolution in the hyperarid Negev Desert, Israel" @default.
• W2017640044 cites W1972016282 @default.
• W2017640044 cites W1972793009 @default.
• W2017640044 cites W1996989815 @default.
• W2017640044 cites W1999798461 @default.
• W2017640044 cites W2003376191 @default.
• W2017640044 cites W2005035365 @default.
• W2017640044 cites W2007711793 @default.
• W2017640044 cites W2016799178 @default.
• W2017640044 cites W2017475051 @default.
• W2017640044 cites W2018023419 @default.
• W2017640044 cites W2020679039 @default.
• W2017640044 cites W2031880607 @default.
• W2017640044 cites W2032270353 @default.
• W2017640044 cites W2034363526 @default.
• W2017640044 cites W2037026371 @default.
• W2017640044 cites W2046938089 @default.
• W2017640044 cites W2051573140 @default.
• W2017640044 cites W2073524588 @default.
• W2017640044 cites W2074131469 @default.
• W2017640044 cites W2076442566 @default.
• W2017640044 cites W2078734959 @default.
• W2017640044 cites W2079921809 @default.
• W2017640044 cites W2084333192 @default.
• W2017640044 cites W2094408279 @default.
• W2017640044 cites W2098797024 @default.
• W2017640044 cites W2099338989 @default.
• W2017640044 cites W2111996152 @default.
• W2017640044 cites W2119262167 @default.
• W2017640044 cites W2127273188 @default.
• W2017640044 cites W2131642202 @default.
• W2017640044 cites W2141643578 @default.
• W2017640044 cites W2145216970 @default.
• W2017640044 cites W2161176006 @default.
• W2017640044 cites W2168133538 @default.
• W2017640044 cites W2321053471 @default.
• W2017640044 cites W4249264918 @default.
• W2017640044 doi "https://doi.org/10.1016/j.geomorph.2011.07.011" @default.
• W2017640044 hasPublicationYear "2011" @default.
• W2017640044 type Work @default.
• W2017640044 sameAs 2017640044 @default.
• W2017640044 citedByCount "16" @default.
• W2017640044 countsByYear W20176400442012 @default.
• W2017640044 countsByYear W20176400442013 @default.
• W2017640044 countsByYear W20176400442014 @default.
• W2017640044 countsByYear W20176400442016 @default.
• W2017640044 countsByYear W20176400442017 @default.
• W2017640044 countsByYear W20176400442018 @default.
• W2017640044 countsByYear W20176400442019 @default.
• W2017640044 countsByYear W20176400442020 @default.
• W2017640044 countsByYear W20176400442021 @default.
• W2017640044 countsByYear W20176400442023 @default.
• W2017640044 crossrefType "journal-article" @default.
• W2017640044 hasAuthorship W2017640044A5006721636 @default.
• W2017640044 hasAuthorship W2017640044A5014110342 @default.
• W2017640044 hasAuthorship W2017640044A5059267263 @default.
• W2017640044 hasAuthorship W2017640044A5087720865 @default.
• W2017640044 hasConcept C109007969 @default.
• W2017640044 hasConcept C112959462 @default.
• W2017640044 hasConcept C114793014 @default.
• W2017640044 hasConcept C123157820 @default.
• W2017640044 hasConcept C127313418 @default.
• W2017640044 hasConcept C137527640 @default.
• W2017640044 hasConcept C142614818 @default.
• W2017640044 hasConcept C151730666 @default.
• W2017640044 hasConcept C160464908 @default.
• W2017640044 hasConcept C17409809 @default.
• W2017640044 hasConcept C2816523 @default.
• W2017640044 hasConcept C32552466 @default.
• W2017640044 hasConcept C64297162 @default.
• W2017640044 hasConcept C6494504 @default.
• W2017640044 hasConcept C69823785 @default.
• W2017640044 hasConceptScore W2017640044C109007969 @default.
• W2017640044 hasConceptScore W2017640044C112959462 @default.
• W2017640044 hasConceptScore W2017640044C114793014 @default.
• W2017640044 hasConceptScore W2017640044C123157820 @default.
• W2017640044 hasConceptScore W2017640044C127313418 @default.
• W2017640044 hasConceptScore W2017640044C137527640 @default.
• W2017640044 hasConceptScore W2017640044C142614818 @default.
• W2017640044 hasConceptScore W2017640044C151730666 @default.
• W2017640044 hasConceptScore W2017640044C160464908 @default.
• W2017640044 hasConceptScore W2017640044C17409809 @default.
• W2017640044 hasConceptScore W2017640044C2816523 @default.
• W2017640044 hasConceptScore W2017640044C32552466 @default.
• W2017640044 hasConceptScore W2017640044C64297162 @default.
• W2017640044 hasConceptScore W2017640044C6494504 @default.
• W2017640044 hasConceptScore W2017640044C69823785 @default.
• W2017640044 hasIssue "3-4" @default.
• W2017640044 hasLocation W20176400441 @default.
• W2017640044 hasOpenAccess W2017640044 @default.

• next