FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2016086823> ?p ?o ?g. }

• W2016086823 endingPage "349" @default.
• W2016086823 startingPage "331" @default.
• W2016086823 abstract "A variety of near-regional (300 km) data, including spectral amplitudes of Pg, surface-wave forms, and close-in (5-10 km) accelerograms have been used to build an elastic seismic source model for a 1-Mton explosion in tuff at near-regional distances. The model consists of: (1) a pressure pulse which injects 3 × 1012 cm3 of volume into the medium, (2) a vertical, upward force impulse that imparts 1018 dyn-s of momentum to the medium, each source component having a time duration of 0.6 s and a depth of 1.3 km. The force impulse appears to be required by two considerations: (a) the striking similarity, apart from sign, of explosion surface waves with those of their cavity collapses, (b) the observation of considerable SV energy leaving the source of the 1-Mton explosions JORUM and HANDLEY. Scaling curves have been constructed which fit the proposed source model. These scaling curves employ: very slow decrease, as (yield)-0.10 of the primary corner frequency; decay as (frequency)4 or (frequency)3 to high frequency. While these scaling curves are unconventional, they appear to be the only ones which can satisfy the near-regional data. The slow scaling with yield of the spectral carner frequency suggests that it is caused by something other than the equivalent elastic radius, e.g. the time duration of motion at the source. The results, at odds with similar studies at teleseismic distances, suggest that significantly different equivalent elastic sources are required at near-regional (as compared with teleseismic) distances; therefore, the effect of the upward impulse might not be seen at teleseismic distances. Consequently, these results probably do not pertain to the seismic discrimination problem at teleseismic distances." @default.
• W2016086823 created "2016-06-24" @default.
• W2016086823 creator A5067593750 @default.
• W2016086823 date "1977-03-01" @default.
• W2016086823 modified "2023-09-27" @default.
• W2016086823 title "A near-regional explosion source model for tuff" @default.
• W2016086823 cites W1761838173 @default.
• W2016086823 cites W1953969651 @default.
• W2016086823 cites W1980466733 @default.
• W2016086823 cites W1988783481 @default.
• W2016086823 cites W1989647463 @default.
• W2016086823 cites W2026477221 @default.
• W2016086823 cites W2053784339 @default.
• W2016086823 cites W2066258505 @default.
• W2016086823 cites W2085002629 @default.
• W2016086823 cites W2093695906 @default.
• W2016086823 cites W2095970764 @default.
• W2016086823 cites W2105173611 @default.
• W2016086823 cites W2114082636 @default.
• W2016086823 cites W2139518028 @default.
• W2016086823 cites W2146927334 @default.
• W2016086823 cites W2150846593 @default.
• W2016086823 cites W2167138817 @default.
• W2016086823 cites W2331676448 @default.
• W2016086823 doi "https://doi.org/10.1111/j.1365-246x.1977.tb03676.x" @default.
• W2016086823 hasPublicationYear "1977" @default.
• W2016086823 type Work @default.
• W2016086823 sameAs 2016086823 @default.
• W2016086823 citedByCount "3" @default.
• W2016086823 crossrefType "journal-article" @default.
• W2016086823 hasAuthorship W2016086823A5067593750 @default.
• W2016086823 hasBestOaLocation W20160868231 @default.
• W2016086823 hasConcept C120665830 @default.
• W2016086823 hasConcept C121332964 @default.
• W2016086823 hasConcept C127313418 @default.
• W2016086823 hasConcept C165205528 @default.
• W2016086823 hasConcept C169744125 @default.
• W2016086823 hasConcept C178635117 @default.
• W2016086823 hasConcept C180205008 @default.
• W2016086823 hasConcept C2524010 @default.
• W2016086823 hasConcept C2985998994 @default.
• W2016086823 hasConcept C30475298 @default.
• W2016086823 hasConcept C33923547 @default.
• W2016086823 hasConcept C38652104 @default.
• W2016086823 hasConcept C41008148 @default.
• W2016086823 hasConcept C57879066 @default.
• W2016086823 hasConcept C70836080 @default.
• W2016086823 hasConcept C74650414 @default.
• W2016086823 hasConcept C99844830 @default.
• W2016086823 hasConceptScore W2016086823C120665830 @default.
• W2016086823 hasConceptScore W2016086823C121332964 @default.
• W2016086823 hasConceptScore W2016086823C127313418 @default.
• W2016086823 hasConceptScore W2016086823C165205528 @default.
• W2016086823 hasConceptScore W2016086823C169744125 @default.
• W2016086823 hasConceptScore W2016086823C178635117 @default.
• W2016086823 hasConceptScore W2016086823C180205008 @default.
• W2016086823 hasConceptScore W2016086823C2524010 @default.
• W2016086823 hasConceptScore W2016086823C2985998994 @default.
• W2016086823 hasConceptScore W2016086823C30475298 @default.
• W2016086823 hasConceptScore W2016086823C33923547 @default.
• W2016086823 hasConceptScore W2016086823C38652104 @default.
• W2016086823 hasConceptScore W2016086823C41008148 @default.
• W2016086823 hasConceptScore W2016086823C57879066 @default.
• W2016086823 hasConceptScore W2016086823C70836080 @default.
• W2016086823 hasConceptScore W2016086823C74650414 @default.
• W2016086823 hasConceptScore W2016086823C99844830 @default.
• W2016086823 hasIssue "3" @default.
• W2016086823 hasLocation W20160868231 @default.
• W2016086823 hasOpenAccess W2016086823 @default.
• W2016086823 hasPrimaryLocation W20160868231 @default.
• W2016086823 hasRelatedWork W1974929695 @default.
• W2016086823 hasRelatedWork W2016086823 @default.
• W2016086823 hasRelatedWork W2053983673 @default.
• W2016086823 hasRelatedWork W2077971514 @default.
• W2016086823 hasRelatedWork W2094657750 @default.
• W2016086823 hasRelatedWork W2142528281 @default.
• W2016086823 hasRelatedWork W2155809674 @default.
• W2016086823 hasRelatedWork W2171215180 @default.
• W2016086823 hasRelatedWork W2586085291 @default.
• W2016086823 hasRelatedWork W1606664876 @default.
• W2016086823 hasVolume "48" @default.
• W2016086823 isParatext "false" @default.
• W2016086823 isRetracted "false" @default.
• W2016086823 magId "2016086823" @default.
• W2016086823 workType "article" @default.