FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2004490640> ?p ?o ?g. }

• W2004490640 endingPage "51" @default.
• W2004490640 startingPage "36" @default.
• W2004490640 abstract "Abstract A paleomagnetic study has been carried out on a waterlaid detrital sedimentary sequence of ~ 240 cm thick within the Seso Cave System (West-Central Pyrenees). In these sediments, seven charcoal samples were dated using 14C AMS ranging from 2080 to 650 cal yr BP (130 BC–1300 AD). Two levels of human occupation of the cave have been recognized by ceramics associated to the Iberian Period and to the Roman Period, respectively. The detrital sedimentary sequence is made of autochthonous (piping detached material from the Eocene marls host rock inside of the cavity) and allochthonous (stream transported sediments from the outside) sediments. The autochthonous material (first 100 cm), made of fine grain laminated sediments (lutites and marls) corresponds to pond facies; the allochthonous material (190–240 cm) is made of lutites and sands and corresponds to stream facies, and both facies are mixed from 100 to 190 cm. The increase in sedimentation rate towards the end of the sequence (stream facies) points to an intensification of the alluvial activity as a possible consequence of a more arid climate during the Medieval Climate Anomaly. For the paleomagnetic study, 44 discrete cylindrical samples were taken along the detrital sequence. The values of the natural remanent magnetization and magnetic susceptibility are significantly lower in the pond sediments than in the stream sediments. The declination and inclination of the paleomagnetic characteristic component (sister samples analyzed by both alternating field and temperature demagnetizing procedure) of each depth point is compared to the Spanish archeomagnetic catalog and available geomagnetic models (ARCH3k.1, CALS3k.4, CALS10k.1b and SCHA.DIF.3K) in order to determine the accuracy of these sediments recording the Earth's magnetic field. Results suggest that these sediments poorly record the Earth's magnetic field, however, paleomagnetic inclination shows similar results between both demagnetizing methods and the inclination is well recorded especially in the younger stream facies. The lack of archeological remains with absolute dates from 925 to 1545 cal yr BP in the Iberian paleomagnetic secular variation reference curve has prevented, up to now, the study of that time period. Therefore, the inclination data from the Seso Cave deposit is the first record of the Iberian paleomagnetic secular variation during most part of the Medieval time, and they are closer to the inclination values of one geomagnetic model (CALS10k.1b)." @default.
• W2004490640 created "2016-06-24" @default.
• W2004490640 creator A5002130187 @default.
• W2004490640 creator A5025405608 @default.
• W2004490640 creator A5026939932 @default.
• W2004490640 creator A5029650332 @default.
• W2004490640 creator A5062070242 @default.
• W2004490640 creator A5072987705 @default.
• W2004490640 creator A5080350363 @default.
• W2004490640 date "2014-08-01" @default.
• W2004490640 modified "2023-10-17" @default.
• W2004490640 title "Testing the reliability of detrital cave sediments as recorders of paleomagnetic secular variations, Seso Cave System (Central Pyrenees, Spain)" @default.
• W2004490640 cites W128593784 @default.
• W2004490640 cites W1507875338 @default.
• W2004490640 cites W1579553792 @default.
• W2004490640 cites W1973723073 @default.
• W2004490640 cites W1974119792 @default.
• W2004490640 cites W1974778563 @default.
• W2004490640 cites W1978313220 @default.
• W2004490640 cites W1986684961 @default.
• W2004490640 cites W1998878851 @default.
• W2004490640 cites W2016651782 @default.
• W2004490640 cites W2033117475 @default.
• W2004490640 cites W2040562495 @default.
• W2004490640 cites W2046511317 @default.
• W2004490640 cites W2050426909 @default.
• W2004490640 cites W2051900611 @default.
• W2004490640 cites W2053250359 @default.
• W2004490640 cites W2065645449 @default.
• W2004490640 cites W2071842791 @default.
• W2004490640 cites W2078374029 @default.
• W2004490640 cites W2086739357 @default.
• W2004490640 cites W2088688901 @default.
• W2004490640 cites W2094584790 @default.
• W2004490640 cites W2094646879 @default.
• W2004490640 cites W2103392376 @default.
• W2004490640 cites W2118204502 @default.
• W2004490640 cites W2122559396 @default.
• W2004490640 cites W2124730454 @default.
• W2004490640 cites W2129925850 @default.
• W2004490640 cites W2133449723 @default.
• W2004490640 cites W2138003187 @default.
• W2004490640 cites W2147458491 @default.
• W2004490640 cites W2159454800 @default.
• W2004490640 cites W4246027503 @default.
• W2004490640 cites W4249751050 @default.
• W2004490640 doi "https://doi.org/10.1016/j.catena.2014.03.009" @default.
• W2004490640 hasPublicationYear "2014" @default.
• W2004490640 type Work @default.
• W2004490640 sameAs 2004490640 @default.
• W2004490640 citedByCount "5" @default.
• W2004490640 countsByYear W20044906402014 @default.
• W2004490640 countsByYear W20044906402015 @default.
• W2004490640 countsByYear W20044906402018 @default.
• W2004490640 countsByYear W20044906402020 @default.
• W2004490640 countsByYear W20044906402021 @default.
• W2004490640 crossrefType "journal-article" @default.
• W2004490640 hasAuthorship W2004490640A5002130187 @default.
• W2004490640 hasAuthorship W2004490640A5025405608 @default.
• W2004490640 hasAuthorship W2004490640A5026939932 @default.
• W2004490640 hasAuthorship W2004490640A5029650332 @default.
• W2004490640 hasAuthorship W2004490640A5062070242 @default.
• W2004490640 hasAuthorship W2004490640A5072987705 @default.
• W2004490640 hasAuthorship W2004490640A5080350363 @default.
• W2004490640 hasBestOaLocation W20044906402 @default.
• W2004490640 hasConcept C112197492 @default.
• W2004490640 hasConcept C114793014 @default.
• W2004490640 hasConcept C115260700 @default.
• W2004490640 hasConcept C121332964 @default.
• W2004490640 hasConcept C127313418 @default.
• W2004490640 hasConcept C149951536 @default.
• W2004490640 hasConcept C151730666 @default.
• W2004490640 hasConcept C166957645 @default.
• W2004490640 hasConcept C170641098 @default.
• W2004490640 hasConcept C171878925 @default.
• W2004490640 hasConcept C189479680 @default.
• W2004490640 hasConcept C199635899 @default.
• W2004490640 hasConcept C205649164 @default.
• W2004490640 hasConcept C62520636 @default.
• W2004490640 hasConcept C8058405 @default.
• W2004490640 hasConceptScore W2004490640C112197492 @default.
• W2004490640 hasConceptScore W2004490640C114793014 @default.
• W2004490640 hasConceptScore W2004490640C115260700 @default.
• W2004490640 hasConceptScore W2004490640C121332964 @default.
• W2004490640 hasConceptScore W2004490640C127313418 @default.
• W2004490640 hasConceptScore W2004490640C149951536 @default.
• W2004490640 hasConceptScore W2004490640C151730666 @default.
• W2004490640 hasConceptScore W2004490640C166957645 @default.
• W2004490640 hasConceptScore W2004490640C170641098 @default.
• W2004490640 hasConceptScore W2004490640C171878925 @default.
• W2004490640 hasConceptScore W2004490640C189479680 @default.
• W2004490640 hasConceptScore W2004490640C199635899 @default.
• W2004490640 hasConceptScore W2004490640C205649164 @default.
• W2004490640 hasConceptScore W2004490640C62520636 @default.
• W2004490640 hasConceptScore W2004490640C8058405 @default.
• W2004490640 hasLocation W20044906401 @default.
• W2004490640 hasLocation W20044906402 @default.
• W2004490640 hasOpenAccess W2004490640 @default.

• next