FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1568278051> ?p ?o ?g. }

• W1568278051 endingPage "813" @default.
• W1568278051 startingPage "808" @default.
• W1568278051 abstract "[1] We use ambient-noise tomography to map regional differences in crustal Rayleigh-wave group velocities with periods of 8–40 s across north Tibet using the International Deep Profiling of Tibet and the Himalaya phase IV arrays (132 stations, deployed for 10–24 months). For periods of 8–24 s (sensitive to midcrustal depths of ~5–30 km), we observe striking velocity changes across the Bangong-Nujiang and Jinsha suture zones as well as the Kunlun-Qaidam boundary. From south to north, we see higher velocities beneath the Lhasa terrane, lower velocities beneath the Qiangtang, higher velocities in the Songpan-Ganzi and Kunlun terranes, and the lowest velocities beneath the Qaidam Basin. Maps at periods of 34 and 40 s (sensitive to the middle and lower crust at depths of ~30–60 km) do not show evidence of changes across those boundaries. Any differences between the Tibetan terrane lower crusts that were present at accretion have been erased or displaced by Cenozoic processes and replaced almost ubiquitously by uniformly low velocities." @default.
• W1568278051 created "2016-06-24" @default.
• W1568278051 creator A5027283087 @default.
• W1568278051 creator A5045665649 @default.
• W1568278051 creator A5059406290 @default.
• W1568278051 creator A5063415227 @default.
• W1568278051 creator A5065126752 @default.
• W1568278051 creator A5068663349 @default.
• W1568278051 creator A5070951223 @default.
• W1568278051 creator A5082049968 @default.
• W1568278051 date "2013-03-06" @default.
• W1568278051 modified "2023-09-29" @default.
• W1568278051 title "Ambient-noise tomography of north Tibet limits geological terrane signature to upper-middle crust" @default.
• W1568278051 cites W1483211514 @default.
• W1568278051 cites W1668496788 @default.
• W1568278051 cites W1771026761 @default.
• W1568278051 cites W1845341270 @default.
• W1568278051 cites W1873025507 @default.
• W1568278051 cites W1899228812 @default.
• W1568278051 cites W1973250961 @default.
• W1568278051 cites W1978299514 @default.
• W1568278051 cites W1997744066 @default.
• W1568278051 cites W2021029412 @default.
• W1568278051 cites W2029660105 @default.
• W1568278051 cites W2034822468 @default.
• W1568278051 cites W2049605743 @default.
• W1568278051 cites W2083213653 @default.
• W1568278051 cites W2090062364 @default.
• W1568278051 cites W2097897435 @default.
• W1568278051 cites W2099307303 @default.
• W1568278051 cites W2104680596 @default.
• W1568278051 cites W2113319450 @default.
• W1568278051 cites W2113585222 @default.
• W1568278051 cites W2116027322 @default.
• W1568278051 cites W2123355107 @default.
• W1568278051 cites W2132517126 @default.
• W1568278051 cites W2139081351 @default.
• W1568278051 cites W2139713088 @default.
• W1568278051 cites W2141240672 @default.
• W1568278051 cites W2144321410 @default.
• W1568278051 cites W2144583290 @default.
• W1568278051 cites W2148418336 @default.
• W1568278051 cites W2170810558 @default.
• W1568278051 cites W2213957681 @default.
• W1568278051 doi "https://doi.org/10.1002/grl.50202" @default.
• W1568278051 hasPublicationYear "2013" @default.
• W1568278051 type Work @default.
• W1568278051 sameAs 1568278051 @default.
• W1568278051 citedByCount "19" @default.
• W1568278051 countsByYear W15682780512013 @default.
• W1568278051 countsByYear W15682780512014 @default.
• W1568278051 countsByYear W15682780512015 @default.
• W1568278051 countsByYear W15682780512016 @default.
• W1568278051 countsByYear W15682780512017 @default.
• W1568278051 countsByYear W15682780512018 @default.
• W1568278051 countsByYear W15682780512019 @default.
• W1568278051 countsByYear W15682780512020 @default.
• W1568278051 countsByYear W15682780512021 @default.
• W1568278051 countsByYear W15682780512023 @default.
• W1568278051 crossrefType "journal-article" @default.
• W1568278051 hasAuthorship W1568278051A5027283087 @default.
• W1568278051 hasAuthorship W1568278051A5045665649 @default.
• W1568278051 hasAuthorship W1568278051A5059406290 @default.
• W1568278051 hasAuthorship W1568278051A5063415227 @default.
• W1568278051 hasAuthorship W1568278051A5065126752 @default.
• W1568278051 hasAuthorship W1568278051A5068663349 @default.
• W1568278051 hasAuthorship W1568278051A5070951223 @default.
• W1568278051 hasAuthorship W1568278051A5082049968 @default.
• W1568278051 hasBestOaLocation W15682780512 @default.
• W1568278051 hasConcept C126838900 @default.
• W1568278051 hasConcept C127313418 @default.
• W1568278051 hasConcept C150999391 @default.
• W1568278051 hasConcept C163716698 @default.
• W1568278051 hasConcept C165205528 @default.
• W1568278051 hasConcept C2776698055 @default.
• W1568278051 hasConcept C2994012208 @default.
• W1568278051 hasConcept C71924100 @default.
• W1568278051 hasConcept C77928131 @default.
• W1568278051 hasConcept C8058405 @default.
• W1568278051 hasConceptScore W1568278051C126838900 @default.
• W1568278051 hasConceptScore W1568278051C127313418 @default.
• W1568278051 hasConceptScore W1568278051C150999391 @default.
• W1568278051 hasConceptScore W1568278051C163716698 @default.
• W1568278051 hasConceptScore W1568278051C165205528 @default.
• W1568278051 hasConceptScore W1568278051C2776698055 @default.
• W1568278051 hasConceptScore W1568278051C2994012208 @default.
• W1568278051 hasConceptScore W1568278051C71924100 @default.
• W1568278051 hasConceptScore W1568278051C77928131 @default.
• W1568278051 hasConceptScore W1568278051C8058405 @default.
• W1568278051 hasIssue "5" @default.
• W1568278051 hasLocation W15682780511 @default.
• W1568278051 hasLocation W15682780512 @default.
• W1568278051 hasLocation W15682780513 @default.
• W1568278051 hasOpenAccess W1568278051 @default.
• W1568278051 hasPrimaryLocation W15682780511 @default.
• W1568278051 hasRelatedWork W2050585109 @default.
• W1568278051 hasRelatedWork W2079119359 @default.
• W1568278051 hasRelatedWork W2134654661 @default.

• next