FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2139869904> ?p ?o ?g. }

• W2139869904 endingPage "3824" @default.
• W2139869904 startingPage "3817" @default.
• W2139869904 abstract "Four seismograms obtained during 1958 and 1959 from large quarry blasts at Promontory (1,221,000 and 2,138,000 Ib of explosive) and Lakeside, Utah (1,500,000 Ib), and the underground Blanca nuclear explosion (38,000,000 Ib equivalent) near Mercury, Nevada, were studied to ascertain whether converted waves of PS type were recorded and, if so, whether they could be used in an analysis of earth crustal layering, as proposed by Andreev in 1957. The PS converted wave is presumed to be composed principally of the SV-type wave (vertically polarized shear wave) and to result from the conversion of energy from the parent compressional P wave at the interface between two crustal layers of contrasting seismic velocity. The method of analysis consisted in computing theoretical times of arrival for PS converted waves based on crustal layering and velocities in the area as determined from refraction seismic studies by Berg, Cook, and Narans [1959], by plotting the radial horizontal component versus the vertical component of velocity of ground motion over appropriate time intervals, and by comparing amplitudes and frequencies of the PS converted waves with the amplitude and frequency of the parent P wave. Arrivals, provisionally interpreted as PS converted waves, were detected on the traces of both the radial horizontal-component seismometers (2 cps natural frequency) and the vertical component seismometers (2 cps). The amplitude of the PS converted waves was usually several times greater than that of the first arrival of the P wave. The successively later arrivals of PS converted waves from successively deeper horizons showed progressively greater ground-velocity amplitudes, as found by Andreev on earthquake seismograms, but some variance from this generalization was found. The frequencies of the various PS converted wave arrivals were approximately the same as those of the parent P wave, between 5 and 10 cps. The crustal layering, which was determined by using the times of arrival of the PS converted waves, compared favorably with that given by Berg, Cook, and Narans for this area. The computed depths of the successive layers were: 5.5, 9.7, 16, and 26 km at Neola, Utah (epicentral distance of about 245 km from Lakeside blast); 12, 26, and 31 km at Gold Hill, Utah (173 km from Promontory); 8.6, 24, and 29 km, also at Gold Hill (379 km from Blanca); and 12, 22, and 31 km at Elko, Nevada (279 km from Promontory)." @default.
• W2139869904 created "2016-06-24" @default.
• W2139869904 creator A5011238808 @default.
• W2139869904 creator A5067024390 @default.
• W2139869904 creator A5082485283 @default.
• W2139869904 date "1960-11-01" @default.
• W2139869904 modified "2023-10-08" @default.
• W2139869904 title "<i>PS</i>converted waves from large explosions" @default.
• W2139869904 cites W4238034646 @default.
• W2139869904 doi "https://doi.org/10.1029/jz065i011p03817" @default.
• W2139869904 hasPublicationYear "1960" @default.
• W2139869904 type Work @default.
• W2139869904 sameAs 2139869904 @default.
• W2139869904 citedByCount "11" @default.
• W2139869904 countsByYear W21398699042013 @default.
• W2139869904 countsByYear W21398699042022 @default.
• W2139869904 crossrefType "journal-article" @default.
• W2139869904 hasAuthorship W2139869904A5011238808 @default.
• W2139869904 hasAuthorship W2139869904A5067024390 @default.
• W2139869904 hasAuthorship W2139869904A5082485283 @default.
• W2139869904 hasConcept C119217923 @default.
• W2139869904 hasConcept C120665830 @default.
• W2139869904 hasConcept C121332964 @default.
• W2139869904 hasConcept C127313418 @default.
• W2139869904 hasConcept C143351421 @default.
• W2139869904 hasConcept C154238967 @default.
• W2139869904 hasConcept C164705383 @default.
• W2139869904 hasConcept C165205528 @default.
• W2139869904 hasConcept C16541007 @default.
• W2139869904 hasConcept C169744125 @default.
• W2139869904 hasConcept C176055353 @default.
• W2139869904 hasConcept C178790620 @default.
• W2139869904 hasConcept C180205008 @default.
• W2139869904 hasConcept C185592680 @default.
• W2139869904 hasConcept C2779161974 @default.
• W2139869904 hasConcept C2993348884 @default.
• W2139869904 hasConcept C39557679 @default.
• W2139869904 hasConcept C43179477 @default.
• W2139869904 hasConcept C44886760 @default.
• W2139869904 hasConcept C51473458 @default.
• W2139869904 hasConcept C59822182 @default.
• W2139869904 hasConcept C71924100 @default.
• W2139869904 hasConcept C7266685 @default.
• W2139869904 hasConcept C78542244 @default.
• W2139869904 hasConcept C8058405 @default.
• W2139869904 hasConcept C84174578 @default.
• W2139869904 hasConcept C86803240 @default.
• W2139869904 hasConceptScore W2139869904C119217923 @default.
• W2139869904 hasConceptScore W2139869904C120665830 @default.
• W2139869904 hasConceptScore W2139869904C121332964 @default.
• W2139869904 hasConceptScore W2139869904C127313418 @default.
• W2139869904 hasConceptScore W2139869904C143351421 @default.
• W2139869904 hasConceptScore W2139869904C154238967 @default.
• W2139869904 hasConceptScore W2139869904C164705383 @default.
• W2139869904 hasConceptScore W2139869904C165205528 @default.
• W2139869904 hasConceptScore W2139869904C16541007 @default.
• W2139869904 hasConceptScore W2139869904C169744125 @default.
• W2139869904 hasConceptScore W2139869904C176055353 @default.
• W2139869904 hasConceptScore W2139869904C178790620 @default.
• W2139869904 hasConceptScore W2139869904C180205008 @default.
• W2139869904 hasConceptScore W2139869904C185592680 @default.
• W2139869904 hasConceptScore W2139869904C2779161974 @default.
• W2139869904 hasConceptScore W2139869904C2993348884 @default.
• W2139869904 hasConceptScore W2139869904C39557679 @default.
• W2139869904 hasConceptScore W2139869904C43179477 @default.
• W2139869904 hasConceptScore W2139869904C44886760 @default.
• W2139869904 hasConceptScore W2139869904C51473458 @default.
• W2139869904 hasConceptScore W2139869904C59822182 @default.
• W2139869904 hasConceptScore W2139869904C71924100 @default.
• W2139869904 hasConceptScore W2139869904C7266685 @default.
• W2139869904 hasConceptScore W2139869904C78542244 @default.
• W2139869904 hasConceptScore W2139869904C8058405 @default.
• W2139869904 hasConceptScore W2139869904C84174578 @default.
• W2139869904 hasConceptScore W2139869904C86803240 @default.
• W2139869904 hasIssue "11" @default.
• W2139869904 hasLocation W21398699041 @default.
• W2139869904 hasOpenAccess W2139869904 @default.
• W2139869904 hasPrimaryLocation W21398699041 @default.
• W2139869904 hasRelatedWork W1246875318 @default.
• W2139869904 hasRelatedWork W2030618463 @default.
• W2139869904 hasRelatedWork W2073140861 @default.
• W2139869904 hasRelatedWork W2103891344 @default.
• W2139869904 hasRelatedWork W2118759974 @default.
• W2139869904 hasRelatedWork W2275591791 @default.
• W2139869904 hasRelatedWork W2475312993 @default.
• W2139869904 hasRelatedWork W4211206864 @default.
• W2139869904 hasRelatedWork W4253961052 @default.
• W2139869904 hasRelatedWork W4387349994 @default.
• W2139869904 hasVolume "65" @default.
• W2139869904 isParatext "false" @default.
• W2139869904 isRetracted "false" @default.
• W2139869904 magId "2139869904" @default.
• W2139869904 workType "article" @default.