FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000961119> ?p ?o ?g. }

• W2000961119 endingPage "132" @default.
• W2000961119 startingPage "124" @default.
• W2000961119 abstract "Little information is available on the paleoclimate evolution of northeast Iran relating to global cold and warm stages. The loess/paleosol sequences from southern Mashhad and Kalat-e Naderi areas were studied to determine the landscape evolution and to set up the first chronological framework for the Pleistocene deposits in northeast Iran. The loess deposits in these areas are less thick (up to 12 m) and have a more patchy distribution than in the Caspian Lowland of northern Iran. Infrared stimulated luminescence (IRSL) dating of loess or loess derivatives from the Robat-e Khakestari, Tappeh Salam and Deh Gheybi sections (a) and (b) from southern Mashhad, as well as Kalat-e Naderi sections (a) and (b) in Kalat-e Naderi area provides a more reliable chronological framework for climate and environmental changes taken place over for the time period including the penultimate and last interglacial/glacial cycles. The Robat-e Khakestari section, the Kalat-e Naderi sections (a) and (b), and to some extent the Tappeh Salam section include loess/paleosol sequences, which are chronologically in excellent agreement with the loess record of the Caspian Lowland in northern Iran. The Deh Gheybi sections (a) and (b) include loess-like sediments and fluvial deposits that make their interpretation difficult. Loess accumulated during MIS 2 at the Robat-e Khakestari section and at the Kalat-e Naderi sections (a) and (b) suggesting a more windy and arid Last Glacial Maximum (LGM) in northeast Iran. Paleosols, correlating most likely with MIS 5, were covered by fluvial sediments at the Kalat-e Naderi section (a). The absence of loess deposits correlating to MIS 3 and MIS 4 at the Robat-e Khakestari section is very likely to have been caused by fluvial processes and water erosion." @default.
• W2000961119 created "2016-06-24" @default.
• W2000961119 creator A5006619075 @default.
• W2000961119 creator A5027466575 @default.
• W2000961119 creator A5074035158 @default.
• W2000961119 creator A5086135319 @default.
• W2000961119 creator A5088520786 @default.
• W2000961119 date "2011-04-01" @default.
• W2000961119 modified "2023-09-26" @default.
• W2000961119 title "Chronostratigraphy of loess deposits in northeast Iran" @default.
• W2000961119 cites W1969576931 @default.
• W2000961119 cites W1970069920 @default.
• W2000961119 cites W1976180689 @default.
• W2000961119 cites W1976405908 @default.
• W2000961119 cites W1977297193 @default.
• W2000961119 cites W1977370485 @default.
• W2000961119 cites W1980425636 @default.
• W2000961119 cites W1982952398 @default.
• W2000961119 cites W1993890614 @default.
• W2000961119 cites W2002566699 @default.
• W2000961119 cites W2019391725 @default.
• W2000961119 cites W2029597290 @default.
• W2000961119 cites W2030176397 @default.
• W2000961119 cites W2030907673 @default.
• W2000961119 cites W2033057434 @default.
• W2000961119 cites W2035304876 @default.
• W2000961119 cites W2037147955 @default.
• W2000961119 cites W2038947148 @default.
• W2000961119 cites W2042422241 @default.
• W2000961119 cites W2044733882 @default.
• W2000961119 cites W2049700763 @default.
• W2000961119 cites W2054833444 @default.
• W2000961119 cites W2064255917 @default.
• W2000961119 cites W2068579852 @default.
• W2000961119 cites W2071210836 @default.
• W2000961119 cites W2073160037 @default.
• W2000961119 cites W2074408994 @default.
• W2000961119 cites W2077246746 @default.
• W2000961119 cites W2077275603 @default.
• W2000961119 cites W2079168010 @default.
• W2000961119 cites W2090699423 @default.
• W2000961119 cites W2146605432 @default.
• W2000961119 cites W2154282956 @default.
• W2000961119 doi "https://doi.org/10.1016/j.quaint.2009.08.002" @default.
• W2000961119 hasPublicationYear "2011" @default.
• W2000961119 type Work @default.
• W2000961119 sameAs 2000961119 @default.
• W2000961119 citedByCount "45" @default.
• W2000961119 countsByYear W20009611192013 @default.
• W2000961119 countsByYear W20009611192014 @default.
• W2000961119 countsByYear W20009611192015 @default.
• W2000961119 countsByYear W20009611192016 @default.
• W2000961119 countsByYear W20009611192017 @default.
• W2000961119 countsByYear W20009611192018 @default.
• W2000961119 countsByYear W20009611192019 @default.
• W2000961119 countsByYear W20009611192020 @default.
• W2000961119 countsByYear W20009611192021 @default.
• W2000961119 countsByYear W20009611192022 @default.
• W2000961119 countsByYear W20009611192023 @default.
• W2000961119 crossrefType "journal-article" @default.
• W2000961119 hasAuthorship W2000961119A5006619075 @default.
• W2000961119 hasAuthorship W2000961119A5027466575 @default.
• W2000961119 hasAuthorship W2000961119A5074035158 @default.
• W2000961119 hasAuthorship W2000961119A5086135319 @default.
• W2000961119 hasAuthorship W2000961119A5088520786 @default.
• W2000961119 hasConcept C100970517 @default.
• W2000961119 hasConcept C127313418 @default.
• W2000961119 hasConcept C151730666 @default.
• W2000961119 hasConcept C166957645 @default.
• W2000961119 hasConcept C17409809 @default.
• W2000961119 hasConcept C185515318 @default.
• W2000961119 hasConcept C192797867 @default.
• W2000961119 hasConcept C205649164 @default.
• W2000961119 hasConcept C6494504 @default.
• W2000961119 hasConceptScore W2000961119C100970517 @default.
• W2000961119 hasConceptScore W2000961119C127313418 @default.
• W2000961119 hasConceptScore W2000961119C151730666 @default.
• W2000961119 hasConceptScore W2000961119C166957645 @default.
• W2000961119 hasConceptScore W2000961119C17409809 @default.
• W2000961119 hasConceptScore W2000961119C185515318 @default.
• W2000961119 hasConceptScore W2000961119C192797867 @default.
• W2000961119 hasConceptScore W2000961119C205649164 @default.
• W2000961119 hasConceptScore W2000961119C6494504 @default.
• W2000961119 hasIssue "1-2" @default.
• W2000961119 hasLocation W20009611191 @default.
• W2000961119 hasOpenAccess W2000961119 @default.
• W2000961119 hasPrimaryLocation W20009611191 @default.
• W2000961119 hasRelatedWork W1979277175 @default.
• W2000961119 hasRelatedWork W1987632498 @default.
• W2000961119 hasRelatedWork W1995557122 @default.
• W2000961119 hasRelatedWork W2059342627 @default.
• W2000961119 hasRelatedWork W2095921784 @default.
• W2000961119 hasRelatedWork W2146151718 @default.
• W2000961119 hasRelatedWork W2325683709 @default.
• W2000961119 hasRelatedWork W2331060621 @default.
• W2000961119 hasRelatedWork W3146725882 @default.
• W2000961119 hasRelatedWork W4236622866 @default.
• W2000961119 hasVolume "234" @default.

• next