FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2138838819> ?p ?o ?g. }

• W2138838819 endingPage "442" @default.
• W2138838819 startingPage "431" @default.
• W2138838819 abstract "We report the results of a detailed rock-magnetic study of basaltic andesites for one of the best documented cases of the first occurrence of a new volcano, the 1943–1952 eruption of Paricutin in central Mexico. 102 oriented standard palaeomagnetic cores corresponding to 12 sites were collected from seven different lava effusion episodes, which cover the interval between 1943 September–December and 1946 March–August. Thermomagnetic investigations reveal that remanence is carried in most cases by Ti-poor titanomagnetite, resulting from oxy-exsolution that probably occurred during the initial flow cooling. Unblocking temperature and coercivity, point to ‘small’ pseudo-single domain magnetic grains for these (titano)magnetites. Thermal and alternating field demagnetization indicates that the lavas are characterized by univectorial or two-component magnetizations. Site-mean declinations and inclinations range from 331.9° to 32.3° and from 17.6° to 51.3°, respectively. The overall mean direction for 12 sites is: Dec = 1.8°, Inc = 37.5°, k= 26 and α95= 8.7°. 23 samples were pre-selected for Thellier palaeointensity experiments because of their stable remanent magnetization and relatively low within site dispersion. Thellier palaeointensity experiments have yielded widely dispersed palaeointensity values from the historically observed geomagnetic intensity. Although, individual specimens yielded technically high quality palaeointensity results, the values obtained are significantly different from the expected value of approximately 45 μT." @default.
• W2138838819 created "2016-06-24" @default.
• W2138838819 creator A5001185209 @default.
• W2138838819 creator A5020957593 @default.
• W2138838819 creator A5024214437 @default.
• W2138838819 creator A5044316571 @default.
• W2138838819 creator A5080526883 @default.
• W2138838819 date "2004-03-01" @default.
• W2138838819 modified "2023-10-11" @default.
• W2138838819 title "Palaeomagnetic, rock-magnetic and microscopy studies of historic lava flows from the Paricutin volcano, Mexico: implications for the deflection of palaeomagnetic directions" @default.
• W2138838819 cites W1965251128 @default.
• W2138838819 cites W1967213667 @default.
• W2138838819 cites W1984765308 @default.
• W2138838819 cites W1990345990 @default.
• W2138838819 cites W1995333776 @default.
• W2138838819 cites W1999673370 @default.
• W2138838819 cites W2000541322 @default.
• W2138838819 cites W2001843504 @default.
• W2138838819 cites W2015273388 @default.
• W2138838819 cites W2018709648 @default.
• W2138838819 cites W2020918744 @default.
• W2138838819 cites W2025063289 @default.
• W2138838819 cites W2035634938 @default.
• W2138838819 cites W2040465419 @default.
• W2138838819 cites W2045144341 @default.
• W2138838819 cites W2045400743 @default.
• W2138838819 cites W2047766041 @default.
• W2138838819 cites W2052128667 @default.
• W2138838819 cites W2062349922 @default.
• W2138838819 cites W2085496108 @default.
• W2138838819 cites W2098488874 @default.
• W2138838819 cites W2100616244 @default.
• W2138838819 cites W2131044660 @default.
• W2138838819 cites W2137140691 @default.
• W2138838819 cites W2154707884 @default.
• W2138838819 cites W2159638517 @default.
• W2138838819 cites W2169186946 @default.
• W2138838819 cites W2330476109 @default.
• W2138838819 cites W4242249832 @default.
• W2138838819 cites W2052715038 @default.
• W2138838819 doi "https://doi.org/10.1111/j.1365-246x.2004.02166.x" @default.
• W2138838819 hasPublicationYear "2004" @default.
• W2138838819 type Work @default.
• W2138838819 sameAs 2138838819 @default.
• W2138838819 citedByCount "30" @default.
• W2138838819 countsByYear W21388388192012 @default.
• W2138838819 countsByYear W21388388192014 @default.
• W2138838819 countsByYear W21388388192016 @default.
• W2138838819 countsByYear W21388388192018 @default.
• W2138838819 countsByYear W21388388192019 @default.
• W2138838819 countsByYear W21388388192020 @default.
• W2138838819 countsByYear W21388388192021 @default.
• W2138838819 countsByYear W21388388192022 @default.
• W2138838819 crossrefType "journal-article" @default.
• W2138838819 hasAuthorship W2138838819A5001185209 @default.
• W2138838819 hasAuthorship W2138838819A5020957593 @default.
• W2138838819 hasAuthorship W2138838819A5024214437 @default.
• W2138838819 hasAuthorship W2138838819A5044316571 @default.
• W2138838819 hasAuthorship W2138838819A5080526883 @default.
• W2138838819 hasBestOaLocation W21388388191 @default.
• W2138838819 hasConcept C113754120 @default.
• W2138838819 hasConcept C115260700 @default.
• W2138838819 hasConcept C120806208 @default.
• W2138838819 hasConcept C121332964 @default.
• W2138838819 hasConcept C127313418 @default.
• W2138838819 hasConcept C155058782 @default.
• W2138838819 hasConcept C161509811 @default.
• W2138838819 hasConcept C165205528 @default.
• W2138838819 hasConcept C171782412 @default.
• W2138838819 hasConcept C189479680 @default.
• W2138838819 hasConcept C192241223 @default.
• W2138838819 hasConcept C199635899 @default.
• W2138838819 hasConcept C30893345 @default.
• W2138838819 hasConcept C32546565 @default.
• W2138838819 hasConcept C505970983 @default.
• W2138838819 hasConcept C5900021 @default.
• W2138838819 hasConcept C60434167 @default.
• W2138838819 hasConcept C62520636 @default.
• W2138838819 hasConcept C8058405 @default.
• W2138838819 hasConceptScore W2138838819C113754120 @default.
• W2138838819 hasConceptScore W2138838819C115260700 @default.
• W2138838819 hasConceptScore W2138838819C120806208 @default.
• W2138838819 hasConceptScore W2138838819C121332964 @default.
• W2138838819 hasConceptScore W2138838819C127313418 @default.
• W2138838819 hasConceptScore W2138838819C155058782 @default.
• W2138838819 hasConceptScore W2138838819C161509811 @default.
• W2138838819 hasConceptScore W2138838819C165205528 @default.
• W2138838819 hasConceptScore W2138838819C171782412 @default.
• W2138838819 hasConceptScore W2138838819C189479680 @default.
• W2138838819 hasConceptScore W2138838819C192241223 @default.
• W2138838819 hasConceptScore W2138838819C199635899 @default.
• W2138838819 hasConceptScore W2138838819C30893345 @default.
• W2138838819 hasConceptScore W2138838819C32546565 @default.
• W2138838819 hasConceptScore W2138838819C505970983 @default.
• W2138838819 hasConceptScore W2138838819C5900021 @default.
• W2138838819 hasConceptScore W2138838819C60434167 @default.
• W2138838819 hasConceptScore W2138838819C62520636 @default.
• W2138838819 hasConceptScore W2138838819C8058405 @default.

• next