FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2014131495> ?p ?o ?g. }

• W2014131495 endingPage "57" @default.
• W2014131495 startingPage "43" @default.
• W2014131495 abstract "Landscape evolution is the result of a variety of geomorphological processes and their controls in time. In southern Spain tectonics, climate and sea-level fluctuations have been some of the main variables controlling long-term (Late Cenozoic) landscape evolution. In the Guadalhorce valley, Malaga, geomorphological reconstructions can be undertaken using sedimentary evidence from marine and fluvial deposits as well as erosional evidence such as terrain form and longitudinal profile analysis. Data are obtained and analysed from the Upper Miocene to present. These allow reconstructions which add information and constraints to the uplift history and landscape development of the area. Main sedimentation phases are the Late Tortonian, Early Pliocene and Pleistocene. Important erosional hiatus are found for the Middle Miocene, Messinian and Late Pliocene to Early Pleistocene. These phases of erosion and sedimentation resulted in a relative large and elongated Tortonian marine valley filled with complex sedimentary structures. Next, a prolonged stage of erosion of these deposits and incision of the major valley system took place during the Messinian. In the Pliocene, a short palaeo-Guadalhorce, in a narrow and much smaller valley existed. This valley was partly filled with marine sediments and prograding fan delta complexes. During the Pleistocene, a wider and larger incising river system resulted in rearrangements of the drainage network. Evaluating the uplift history of the area, we found that rates of tectonic activity were higher during the Tortonian–Messinian and Upper Pleistocene, while tectonic activity was lower during the Pliocene. Relative uplift rates for the study area range for the Messinian between 160 and 276 m Ma−1, for the Pliocene between 10 and 15 m Ma−1 and for the Pleistocene between 40 and 100 m Ma−1." @default.
• W2014131495 created "2016-06-24" @default.
• W2014131495 creator A5029773701 @default.
• W2014131495 creator A5061800499 @default.
• W2014131495 date "2003-02-01" @default.
• W2014131495 modified "2023-10-07" @default.
• W2014131495 title "Late Cenozoic landscape development and its tectonic implications for the Guadalhorce valley near Álora (Southern Spain)" @default.
• W2014131495 cites W1965832912 @default.
• W2014131495 cites W1972192371 @default.
• W2014131495 cites W1997189276 @default.
• W2014131495 cites W1997252211 @default.
• W2014131495 cites W1998450920 @default.
• W2014131495 cites W2000930026 @default.
• W2014131495 cites W2005890791 @default.
• W2014131495 cites W2008257245 @default.
• W2014131495 cites W2013141421 @default.
• W2014131495 cites W2019504758 @default.
• W2014131495 cites W2026889119 @default.
• W2014131495 cites W2032130922 @default.
• W2014131495 cites W2047561798 @default.
• W2014131495 cites W2065135402 @default.
• W2014131495 cites W2065983910 @default.
• W2014131495 cites W2067154976 @default.
• W2014131495 cites W2068442114 @default.
• W2014131495 cites W2070044181 @default.
• W2014131495 cites W2087828802 @default.
• W2014131495 cites W2111151668 @default.
• W2014131495 cites W2112828972 @default.
• W2014131495 cites W2130471535 @default.
• W2014131495 cites W2130994975 @default.
• W2014131495 cites W2133346363 @default.
• W2014131495 cites W2134880572 @default.
• W2014131495 cites W2140893622 @default.
• W2014131495 cites W2152867863 @default.
• W2014131495 doi "https://doi.org/10.1016/s0169-555x(02)00207-6" @default.
• W2014131495 hasPublicationYear "2003" @default.
• W2014131495 type Work @default.
• W2014131495 sameAs 2014131495 @default.
• W2014131495 citedByCount "32" @default.
• W2014131495 countsByYear W20141314952012 @default.
• W2014131495 countsByYear W20141314952014 @default.
• W2014131495 countsByYear W20141314952015 @default.
• W2014131495 countsByYear W20141314952016 @default.
• W2014131495 countsByYear W20141314952017 @default.
• W2014131495 countsByYear W20141314952019 @default.
• W2014131495 countsByYear W20141314952020 @default.
• W2014131495 countsByYear W20141314952021 @default.
• W2014131495 countsByYear W20141314952022 @default.
• W2014131495 crossrefType "journal-article" @default.
• W2014131495 hasAuthorship W2014131495A5029773701 @default.
• W2014131495 hasAuthorship W2014131495A5061800499 @default.
• W2014131495 hasConcept C109007969 @default.
• W2014131495 hasConcept C111368507 @default.
• W2014131495 hasConcept C112959462 @default.
• W2014131495 hasConcept C114793014 @default.
• W2014131495 hasConcept C123157820 @default.
• W2014131495 hasConcept C127313418 @default.
• W2014131495 hasConcept C139419234 @default.
• W2014131495 hasConcept C146357865 @default.
• W2014131495 hasConcept C151730666 @default.
• W2014131495 hasConcept C160464908 @default.
• W2014131495 hasConcept C2777775986 @default.
• W2014131495 hasConcept C2779421809 @default.
• W2014131495 hasConcept C53570757 @default.
• W2014131495 hasConcept C6494504 @default.
• W2014131495 hasConcept C73707237 @default.
• W2014131495 hasConcept C74501621 @default.
• W2014131495 hasConcept C77928131 @default.
• W2014131495 hasConceptScore W2014131495C109007969 @default.
• W2014131495 hasConceptScore W2014131495C111368507 @default.
• W2014131495 hasConceptScore W2014131495C112959462 @default.
• W2014131495 hasConceptScore W2014131495C114793014 @default.
• W2014131495 hasConceptScore W2014131495C123157820 @default.
• W2014131495 hasConceptScore W2014131495C127313418 @default.
• W2014131495 hasConceptScore W2014131495C139419234 @default.
• W2014131495 hasConceptScore W2014131495C146357865 @default.
• W2014131495 hasConceptScore W2014131495C151730666 @default.
• W2014131495 hasConceptScore W2014131495C160464908 @default.
• W2014131495 hasConceptScore W2014131495C2777775986 @default.
• W2014131495 hasConceptScore W2014131495C2779421809 @default.
• W2014131495 hasConceptScore W2014131495C53570757 @default.
• W2014131495 hasConceptScore W2014131495C6494504 @default.
• W2014131495 hasConceptScore W2014131495C73707237 @default.
• W2014131495 hasConceptScore W2014131495C74501621 @default.
• W2014131495 hasConceptScore W2014131495C77928131 @default.
• W2014131495 hasIssue "1-3" @default.
• W2014131495 hasLocation W20141314951 @default.
• W2014131495 hasOpenAccess W2014131495 @default.
• W2014131495 hasPrimaryLocation W20141314951 @default.
• W2014131495 hasRelatedWork W1984755569 @default.
• W2014131495 hasRelatedWork W2005853062 @default.
• W2014131495 hasRelatedWork W2014131495 @default.
• W2014131495 hasRelatedWork W2023230246 @default.
• W2014131495 hasRelatedWork W2069297912 @default.
• W2014131495 hasRelatedWork W2088719274 @default.
• W2014131495 hasRelatedWork W2348491433 @default.
• W2014131495 hasRelatedWork W2351834351 @default.
• W2014131495 hasRelatedWork W2387996456 @default.

• next