FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W31905569> ?p ?o ?g. }

• W31905569 endingPage "23" @default.
• W31905569 startingPage "3" @default.
• W31905569 abstract "The attenuation and velocity in the LVZ are linked through the approximate dispersion relation1Q≃π2.dln(modulus)dln(frequence)which holds for all linear attenuation effects regardless of mechanism. The attenuation level alone cannot be used to predict the depression in velocity, but it is reasonable to seek a common explanation for both. Models based on liquid melt pockets in an elastic solid predict attenuation/modulus effects which range widely in magnitude and characteristic frequency, depending critically on the melt geometry. This geometry is at present not known. There is therefore at present no hope of inverting the seismic data to yield melt fraction. Ubiquitous and substantial subsolidus attenuation/modulus effects have been documented for many metals, salts and ceramics; however, it is not possible at present to predict the attenuation level due to this source under upper mantle conditions. The seismic data alone do not permit a choice between a melt or subsolidus explanation for the LVZ. The creep properties of mantle material are certain to be affected by partial melt only if the melt fraction exceeds about 25–30%. Extrapolated laboratory creep data on unmelted olivines are compatible with geophysical evidence of the rheology of the upper mantle. Evidence has accumulated that hydrogen within the olivine lattice (“wet olivine”) leads to mechanical softening. If enough hydrogen can be accommodated in the lattice, it will further complicate the line of reasoning proposed by Wyllie and other petrologists about the melt fraction in the LVZ based on the crystallographic site of mantle water. It appears to this author that no reasonable case can be made at present for any correlation other than empirical between regions of high attenuation, regions of partial melt, and the zone of decoupling of the continents." @default.
• W31905569 created "2016-06-24" @default.
• W31905569 creator A5089842976 @default.
• W31905569 date "1977-01-01" @default.
• W31905569 modified "2023-09-27" @default.
• W31905569 title "A BRIEF SUMMARY OF OUR PRESENT DAY UNDERSTANDING OF THE EFFECT OF VOLATILES AND PARTIAL MELT ON THE MECHANICAL PROPERTIES OF THE UPPER MANTLE" @default.
• W31905569 cites W1496116918 @default.
• W31905569 cites W1508899429 @default.
• W31905569 cites W1536484609 @default.
• W31905569 cites W1648152288 @default.
• W31905569 cites W1966726716 @default.
• W31905569 cites W1970594679 @default.
• W31905569 cites W1974798909 @default.
• W31905569 cites W1977685628 @default.
• W31905569 cites W1980643505 @default.
• W31905569 cites W1983094364 @default.
• W31905569 cites W1986235436 @default.
• W31905569 cites W1987098602 @default.
• W31905569 cites W1993959695 @default.
• W31905569 cites W1999647229 @default.
• W31905569 cites W2000474073 @default.
• W31905569 cites W2000876099 @default.
• W31905569 cites W2009400906 @default.
• W31905569 cites W2009683385 @default.
• W31905569 cites W2010507737 @default.
• W31905569 cites W2012554989 @default.
• W31905569 cites W2015071626 @default.
• W31905569 cites W2015345199 @default.
• W31905569 cites W2019647468 @default.
• W31905569 cites W2021915162 @default.
• W31905569 cites W2027478205 @default.
• W31905569 cites W2031618020 @default.
• W31905569 cites W2037899740 @default.
• W31905569 cites W2045999044 @default.
• W31905569 cites W2047259056 @default.
• W31905569 cites W2047999478 @default.
• W31905569 cites W2051748599 @default.
• W31905569 cites W2055511959 @default.
• W31905569 cites W2055735358 @default.
• W31905569 cites W2057708012 @default.
• W31905569 cites W2058135322 @default.
• W31905569 cites W2059633393 @default.
• W31905569 cites W2064944143 @default.
• W31905569 cites W2065791672 @default.
• W31905569 cites W2067498474 @default.
• W31905569 cites W2071766690 @default.
• W31905569 cites W2073825471 @default.
• W31905569 cites W2080886062 @default.
• W31905569 cites W2083468085 @default.
• W31905569 cites W2087565358 @default.
• W31905569 cites W2088107231 @default.
• W31905569 cites W2089022465 @default.
• W31905569 cites W2091239338 @default.
• W31905569 cites W2096398344 @default.
• W31905569 cites W2111128021 @default.
• W31905569 cites W2116519903 @default.
• W31905569 cites W2124100746 @default.
• W31905569 cites W2127661573 @default.
• W31905569 cites W2136433737 @default.
• W31905569 cites W2138771754 @default.
• W31905569 cites W2159298610 @default.
• W31905569 cites W2164008259 @default.
• W31905569 cites W2264771031 @default.
• W31905569 cites W2283598957 @default.
• W31905569 cites W2318523936 @default.
• W31905569 cites W2479452367 @default.
• W31905569 cites W2764801705 @default.
• W31905569 cites W3139010782 @default.
• W31905569 cites W3185674536 @default.
• W31905569 cites W3194653550 @default.
• W31905569 cites W2100019488 @default.
• W31905569 doi "https://doi.org/10.1016/b978-0-12-468750-9.50007-3" @default.
• W31905569 hasPublicationYear "1977" @default.
• W31905569 type Work @default.
• W31905569 sameAs 31905569 @default.
• W31905569 citedByCount "58" @default.
• W31905569 countsByYear W319055692018 @default.
• W31905569 countsByYear W319055692019 @default.
• W31905569 crossrefType "book-chapter" @default.
• W31905569 hasAuthorship W31905569A5089842976 @default.
• W31905569 hasConcept C120665830 @default.
• W31905569 hasConcept C121332964 @default.
• W31905569 hasConcept C127313418 @default.
• W31905569 hasConcept C159985019 @default.
• W31905569 hasConcept C184652730 @default.
• W31905569 hasConcept C192562407 @default.
• W31905569 hasConcept C199289684 @default.
• W31905569 hasConcept C200990466 @default.
• W31905569 hasConcept C2780364934 @default.
• W31905569 hasConcept C67236022 @default.
• W31905569 hasConcept C8058405 @default.
• W31905569 hasConceptScore W31905569C120665830 @default.
• W31905569 hasConceptScore W31905569C121332964 @default.
• W31905569 hasConceptScore W31905569C127313418 @default.
• W31905569 hasConceptScore W31905569C159985019 @default.
• W31905569 hasConceptScore W31905569C184652730 @default.
• W31905569 hasConceptScore W31905569C192562407 @default.
• W31905569 hasConceptScore W31905569C199289684 @default.

• next