FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1980201210> ?p ?o ?g. }

• W1980201210 endingPage "4424" @default.
• W1980201210 startingPage "4407" @default.
• W1980201210 abstract "A continuous paleomagnetic record for the last 13,000 years was obtained from the sediments of Lake Waiau, located near the summit of Mauna Kea Volcano on the island of Hawaii. The secular variation (SV) of the geomagnetic field was studied using spectral analysis and precession analysis of the magnetic vector. The hypothesis that there has been anomalously low geomagnetic SV in the central Pacific was tested using angular dispersion analysis. The inclination record has a mean value of 27° that is much lower than the 35° predicted by the geocentric axial dipole hypothesis. The spectrum obtained from spectral analysis shows major inclination peaks at periodicities of approximately 3600 and 7900 years and major declination peaks at periodicities of approximately 1100, 2000, 3300, and 7800 years. The approximately 8000‐ and 3500‐year periodicities shown in both inclination and declination spectrums may represent the dipole and nondipole variation, respectively. The approximately 1100‐ and 2000‐year periodicities are probably derived from either the sources that affect declination only or the offsets between the core sections. In addition, Bauer plots of the magnetic vector are dominated by clockwise motion. The angular dispersion calculated from lake sediments is 5.9° with respect to the mean virtual geomagnetic pole (VGP) and 9.1° with respect to the geographic pole. Both values are much lower than the 13.5° expected from paleosecular variation model G which separates the angular dispersion into components from the dipole and the quadruple families. Our results support the hypothesis that an anomalously low secular variation is a characteristic feature of the central Pacific. Furthermore, this geomagnetic behavior persists on time scales of 10 4 years. Regional anomalies in temperature, topography or electrical conductivity at the core‐mantle boundary are inferred to cause the low SV." @default.
• W1980201210 created "2016-06-24" @default.
• W1980201210 creator A5043565689 @default.
• W1980201210 creator A5084111372 @default.
• W1980201210 date "1992-04-10" @default.
• W1980201210 modified "2023-09-27" @default.
• W1980201210 title "A Late Quaternary geomagnetic secular variation record from Lake Waiau, Hawaii, and the question of the Pacific nondipole low" @default.
• W1980201210 cites W138149493 @default.
• W1980201210 cites W1966329790 @default.
• W1980201210 cites W1981870398 @default.
• W1980201210 cites W1996728081 @default.
• W1980201210 cites W1997086424 @default.
• W1980201210 cites W1999673370 @default.
• W1980201210 cites W2001478521 @default.
• W1980201210 cites W2001843504 @default.
• W1980201210 cites W2013003378 @default.
• W1980201210 cites W2013208259 @default.
• W1980201210 cites W2018285375 @default.
• W1980201210 cites W2018910602 @default.
• W1980201210 cites W2020612410 @default.
• W1980201210 cites W2021499629 @default.
• W1980201210 cites W2031342294 @default.
• W1980201210 cites W2034142953 @default.
• W1980201210 cites W2040017715 @default.
• W1980201210 cites W2041730102 @default.
• W1980201210 cites W2047766041 @default.
• W1980201210 cites W2049913572 @default.
• W1980201210 cites W2054943641 @default.
• W1980201210 cites W2079495554 @default.
• W1980201210 cites W2092982142 @default.
• W1980201210 cites W2115291786 @default.
• W1980201210 cites W2124077998 @default.
• W1980201210 cites W2135444961 @default.
• W1980201210 cites W2137177419 @default.
• W1980201210 cites W2138550732 @default.
• W1980201210 cites W2142153850 @default.
• W1980201210 cites W2144567394 @default.
• W1980201210 cites W2145834787 @default.
• W1980201210 cites W2146605432 @default.
• W1980201210 cites W2150537860 @default.
• W1980201210 cites W2155653187 @default.
• W1980201210 cites W2158309032 @default.
• W1980201210 cites W2171002579 @default.
• W1980201210 cites W55882336 @default.
• W1980201210 doi "https://doi.org/10.1029/91jb03074" @default.
• W1980201210 hasPublicationYear "1992" @default.
• W1980201210 type Work @default.
• W1980201210 sameAs 1980201210 @default.
• W1980201210 citedByCount "63" @default.
• W1980201210 countsByYear W19802012102012 @default.
• W1980201210 countsByYear W19802012102013 @default.
• W1980201210 countsByYear W19802012102014 @default.
• W1980201210 countsByYear W19802012102015 @default.
• W1980201210 countsByYear W19802012102016 @default.
• W1980201210 countsByYear W19802012102017 @default.
• W1980201210 countsByYear W19802012102018 @default.
• W1980201210 countsByYear W19802012102020 @default.
• W1980201210 countsByYear W19802012102021 @default.
• W1980201210 countsByYear W19802012102023 @default.
• W1980201210 crossrefType "journal-article" @default.
• W1980201210 hasAuthorship W1980201210A5043565689 @default.
• W1980201210 hasAuthorship W1980201210A5084111372 @default.
• W1980201210 hasConcept C109428209 @default.
• W1980201210 hasConcept C112197492 @default.
• W1980201210 hasConcept C115260700 @default.
• W1980201210 hasConcept C121332964 @default.
• W1980201210 hasConcept C124200008 @default.
• W1980201210 hasConcept C127313418 @default.
• W1980201210 hasConcept C13280743 @default.
• W1980201210 hasConcept C149951536 @default.
• W1980201210 hasConcept C170641098 @default.
• W1980201210 hasConcept C189479680 @default.
• W1980201210 hasConcept C199635899 @default.
• W1980201210 hasConcept C2524010 @default.
• W1980201210 hasConcept C33923547 @default.
• W1980201210 hasConcept C44870925 @default.
• W1980201210 hasConcept C46031176 @default.
• W1980201210 hasConcept C60365795 @default.
• W1980201210 hasConcept C62520636 @default.
• W1980201210 hasConcept C70026782 @default.
• W1980201210 hasConcept C74050887 @default.
• W1980201210 hasConcept C8058405 @default.
• W1980201210 hasConceptScore W1980201210C109428209 @default.
• W1980201210 hasConceptScore W1980201210C112197492 @default.
• W1980201210 hasConceptScore W1980201210C115260700 @default.
• W1980201210 hasConceptScore W1980201210C121332964 @default.
• W1980201210 hasConceptScore W1980201210C124200008 @default.
• W1980201210 hasConceptScore W1980201210C127313418 @default.
• W1980201210 hasConceptScore W1980201210C13280743 @default.
• W1980201210 hasConceptScore W1980201210C149951536 @default.
• W1980201210 hasConceptScore W1980201210C170641098 @default.
• W1980201210 hasConceptScore W1980201210C189479680 @default.
• W1980201210 hasConceptScore W1980201210C199635899 @default.
• W1980201210 hasConceptScore W1980201210C2524010 @default.
• W1980201210 hasConceptScore W1980201210C33923547 @default.
• W1980201210 hasConceptScore W1980201210C44870925 @default.
• W1980201210 hasConceptScore W1980201210C46031176 @default.
• W1980201210 hasConceptScore W1980201210C60365795 @default.

• next