FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2135890651> ?p ?o ?g. }

• W2135890651 endingPage "332" @default.
• W2135890651 startingPage "317" @default.
• W2135890651 abstract "An earlier study of the cyclic Miocene red bed sequence of La Gloria (Spain) by Krijgsman et al. indicated complicated behaviour of the natural remanent magnetization (NRM) in parts of the section, particularly close to reversal boundaries. We resampled part of the section with high resolution and used extensive rock-magnetic analyses to characterize the magnetic remanence carriers. Below a conspicuous hydromorphous layer, the magnetic contributions of haematite and magnetite are approximately equal, while in the brown layers on top of the hydromorphous layer the contribution of magnetite is drastically reduced. This is probably related to a change in hydrological conditions. The NRM is characterized by: (1) a low-temperature (200–360 °C) overprint of unknown age, (2) a medium-temperature (360–580 °C) component, interpreted as the characteristic remanent magnetization (ChRM); and (3) a high-temperature haematite component (600– 680 °C), carrying the same directions as the medium-temperature component. There is no perceivable delay in NRM acquisition between the medium- and the high-temperature components; they are both regarded as primary. The behaviour of the NRM seems to be similar in the cyclic lithologies. The acquisition of NRM thus seems to be independent of lithology in the cyclic part of the section. The higher sampling resolution yielded the detection of a new polarity zone, which probably represents a geomagnetic feature according to rock-magnetic properties. However, the more detailed magnetostratigraphy of the resampled part of the section indicates that the earlier correlation to the geomagnetic polarity timescale is no longer tenable. Therefore, the La Gloria section should no longer be used as a magnetostratigraphic dating tool of mammal biochronology." @default.
• W2135890651 created "2016-06-24" @default.
• W2135890651 creator A5020121884 @default.
• W2135890651 creator A5029653850 @default.
• W2135890651 creator A5045726922 @default.
• W2135890651 creator A5071664024 @default.
• W2135890651 date "2003-05-01" @default.
• W2135890651 modified "2023-09-26" @default.
• W2135890651 title "Rock-magnetic properties of multicomponent natural remanent magnetization in alluvial red beds (NE Spain)" @default.
• W2135890651 cites W1587831682 @default.
• W2135890651 cites W1983989686 @default.
• W2135890651 cites W2003014312 @default.
• W2135890651 cites W2016691163 @default.
• W2135890651 cites W2045044499 @default.
• W2135890651 cites W2048104343 @default.
• W2135890651 cites W2051554077 @default.
• W2135890651 cites W2052635909 @default.
• W2135890651 cites W2061877097 @default.
• W2135890651 cites W2067345100 @default.
• W2135890651 cites W2070011134 @default.
• W2135890651 cites W2072642334 @default.
• W2135890651 cites W2072994970 @default.
• W2135890651 cites W2075155599 @default.
• W2135890651 cites W2076505736 @default.
• W2135890651 cites W2077677977 @default.
• W2135890651 cites W2083555735 @default.
• W2135890651 cites W2092764174 @default.
• W2135890651 cites W2103152441 @default.
• W2135890651 cites W2103416322 @default.
• W2135890651 cites W2105792990 @default.
• W2135890651 cites W2107651592 @default.
• W2135890651 cites W2110695240 @default.
• W2135890651 cites W2118204502 @default.
• W2135890651 cites W2124119288 @default.
• W2135890651 cites W2140250162 @default.
• W2135890651 cites W2144101538 @default.
• W2135890651 cites W2144601518 @default.
• W2135890651 cites W2148545560 @default.
• W2135890651 cites W2150192421 @default.
• W2135890651 cites W2163750858 @default.
• W2135890651 cites W2176167820 @default.
• W2135890651 cites W4205355805 @default.
• W2135890651 doi "https://doi.org/10.1046/j.1365-246x.2003.01880.x" @default.
• W2135890651 hasPublicationYear "2003" @default.
• W2135890651 type Work @default.
• W2135890651 sameAs 2135890651 @default.
• W2135890651 citedByCount "24" @default.
• W2135890651 countsByYear W21358906512012 @default.
• W2135890651 countsByYear W21358906512014 @default.
• W2135890651 countsByYear W21358906512015 @default.
• W2135890651 countsByYear W21358906512016 @default.
• W2135890651 countsByYear W21358906512017 @default.
• W2135890651 countsByYear W21358906512018 @default.
• W2135890651 countsByYear W21358906512019 @default.
• W2135890651 countsByYear W21358906512020 @default.
• W2135890651 countsByYear W21358906512021 @default.
• W2135890651 countsByYear W21358906512022 @default.
• W2135890651 crossrefType "journal-article" @default.
• W2135890651 hasAuthorship W2135890651A5020121884 @default.
• W2135890651 hasAuthorship W2135890651A5029653850 @default.
• W2135890651 hasAuthorship W2135890651A5045726922 @default.
• W2135890651 hasAuthorship W2135890651A5071664024 @default.
• W2135890651 hasConcept C115260700 @default.
• W2135890651 hasConcept C121332964 @default.
• W2135890651 hasConcept C122792734 @default.
• W2135890651 hasConcept C127313418 @default.
• W2135890651 hasConcept C1491633281 @default.
• W2135890651 hasConcept C151730666 @default.
• W2135890651 hasConcept C152406496 @default.
• W2135890651 hasConcept C155058782 @default.
• W2135890651 hasConcept C171782412 @default.
• W2135890651 hasConcept C17409809 @default.
• W2135890651 hasConcept C185592680 @default.
• W2135890651 hasConcept C189479680 @default.
• W2135890651 hasConcept C194482375 @default.
• W2135890651 hasConcept C199289684 @default.
• W2135890651 hasConcept C199635899 @default.
• W2135890651 hasConcept C2777361361 @default.
• W2135890651 hasConcept C2777781897 @default.
• W2135890651 hasConcept C32546565 @default.
• W2135890651 hasConcept C49015763 @default.
• W2135890651 hasConcept C55493867 @default.
• W2135890651 hasConcept C60434167 @default.
• W2135890651 hasConcept C62520636 @default.
• W2135890651 hasConcept C66944017 @default.
• W2135890651 hasConcept C8058405 @default.
• W2135890651 hasConceptScore W2135890651C115260700 @default.
• W2135890651 hasConceptScore W2135890651C121332964 @default.
• W2135890651 hasConceptScore W2135890651C122792734 @default.
• W2135890651 hasConceptScore W2135890651C127313418 @default.
• W2135890651 hasConceptScore W2135890651C1491633281 @default.
• W2135890651 hasConceptScore W2135890651C151730666 @default.
• W2135890651 hasConceptScore W2135890651C152406496 @default.
• W2135890651 hasConceptScore W2135890651C155058782 @default.
• W2135890651 hasConceptScore W2135890651C171782412 @default.
• W2135890651 hasConceptScore W2135890651C17409809 @default.
• W2135890651 hasConceptScore W2135890651C185592680 @default.
• W2135890651 hasConceptScore W2135890651C189479680 @default.

• next