georefid:2000-041399SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1190/1.14445741999-01-01publicationgeorefid:2000-041399doi:10.1190/1.1444574Lizarralde, DanielDanish Lithosphere Center, Copenhagen, DenmarkauthorSwift, SteveWoods Hole Oceanographic Institution, United StatesauthorSociety of Exploration Geophysicists, Tulsa, OK, United StatespublisherdocumentHardcopyGeophysics64 (3)659-661Vertical seismic profile (VSP) direct arrivals provide an insitu measurement of traveltime with depth into the earth. In this note, we describe a weighted, damped least-squares inversion of VSP traveltimes for a smooth velocity/depth function that inherently reveals the resolution of the data. Smooth velocity/depth profiles of this type are suitable for migration or as a starting models for waveform inversion or tomography. The application of this inversion is particularly simple, requiring only the value of the damping parameter to be determined, and this value is determined from residual statistics.completedApplied geophysicsbasaltic compositioncase studiescrustDeep Sea Drilling ProjectdepthDSDP Site 504elastic wavesgeophysical methodsgeophysical profileshigh-resolution methodsinverse problemIPODLeg 111Leg 137Leg 140Leg 148Leg 69Leg 70Leg 83Leg 92Ocean Drilling Programoceanic crustseismic methodsseismic profilesseismic wavestomographytraveltimevelocityvertical seismic profilesurn:org.iodp:exp:111urnlargerWorkCitationcampaignurn:org.iodp:exp:137urnlargerWorkCitationcampaignurn:org.iodp:exp:140urnlargerWorkCitationcampaignurn:org.iodp:exp:148urnlargerWorkCitationcampaignurn:org.iodp:exp:69urnlargerWorkCitationcampaignurn:org.iodp:exp:70urnlargerWorkCitationcampaignurn:org.iodp:exp:83urnlargerWorkCitationcampaignurn:org.iodp:exp:92urnlargerWorkCitationcampaignurn:org.iodp:exp:69:site:504urnlargerWorkCitationstudyurn:org.iodp:exp:69urnlargerWorkCitationcampaignurn:org.iodp:exp:70:site:504urnlargerWorkCitationstudyurn:org.iodp:exp:70urnlargerWorkCitationcampaignurn:org.iodp:exp:83:site:504urnlargerWorkCitationstudyurn:org.iodp:exp:83urnlargerWorkCitationcampaignurn:org.iodp:exp:92:site:504urnlargerWorkCitationstudyurn:org.iodp:exp:92urnlargerWorkCitationcampaignurn:org.iodp:exp:111:site:504urnlargerWorkCitationstudyurn:org.iodp:exp:111urnlargerWorkCitationcampaignurn:org.iodp:exp:137:site:504urnlargerWorkCitationstudyurn:org.iodp:exp:137urnlargerWorkCitationcampaignurn:org.iodp:exp:140:site:504urnlargerWorkCitationstudyurn:org.iodp:exp:140urnlargerWorkCitationcampaignurn:org.iodp:exp:148:site:504urnlargerWorkCitationstudyurn:org.iodp:exp:148urnlargerWorkCitationcampaignEnglishgeoscientificInformation-83.4357-83.43481.13351.1338