FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2078589025> ?p ?o ?g. }

• W2078589025 endingPage "196" @default.
• W2078589025 startingPage "181" @default.
• W2078589025 abstract "The P-wave velocity structure of the upper crust beneath a profile ranging from Niikappu to Samani in the southwestern foot of the Hidaka Mountains, Hokkaido, Japan was obtained through analysis of refraction and wide-angle reflection data. The mountains are characterized by high seismicity and a large gravity anomaly. The present profile crosses the source region of the 1982 Urakawa-oki earthquake (Ms 6.8). The length of the profile is 66 km striking northwest and southeast. Along the profile, 64 vertical geophones were set up and 5 shot points were chosen. For each shot, a 400–600 kg charge of dynamite was detonated. The studied area is composed of four major geological belts: Neogene sedimentary rocks, the Kamuikotan belt, the Yezo Group, and the Hidaka belt. The measurement line crosses these geological trend at an oblique angle. The structure obtained is characterized by remarkable velocity variations in the lateral direction and reflects the surface geological characteristics. A thin, high-velocity layer (HVL) was found between low-velocity materials in the central part of the profile, beneath the Kamuikotan Metamorphic Belt, at a depth ranging from 0.5 to 6 km, overthrusting toward the west on the low-velocity materials consisting of Neogene sedimentary rocks, and forming gentle folds. Outlines of the velocity structure of the Hidaka Mountains yielded by other studies have shown a large-scale overthrust structure associated with the collision of the Outer Kurile and the Outer Northern Honshu Arcs. The shallow velocity structure inferred by the present study showed a similar (although small scale) overthrust structure. The obtained structure shows that the composite tectonic force, comprising westward movement of the Outer Kurile Arc and northward movement of the Outer Northern Honshu Arc, plays an important role in the evolution of the tectonic features of the crust and upper mantle in a wide depth range beneath the Hidaka Mountains." @default.
• W2078589025 created "2016-06-24" @default.
• W2078589025 creator A5004763780 @default.
• W2078589025 creator A5009966291 @default.
• W2078589025 creator A5038522902 @default.
• W2078589025 creator A5055780454 @default.
• W2078589025 creator A5064227339 @default.
• W2078589025 creator A5073974620 @default.
• W2078589025 date "1998-05-01" @default.
• W2078589025 modified "2023-10-03" @default.
• W2078589025 title "Collision structure in the upper crust beneath the southwestern foot of the Hidaka Mountains, Hokkaido, Japan as derived from explosion seismic observations" @default.
• W2078589025 cites W1995812853 @default.
• W2078589025 cites W2003088583 @default.
• W2078589025 cites W2014362192 @default.
• W2078589025 cites W2030139227 @default.
• W2078589025 cites W2032581653 @default.
• W2078589025 cites W2037028262 @default.
• W2078589025 cites W2042256936 @default.
• W2078589025 cites W2051398895 @default.
• W2078589025 cites W2054334560 @default.
• W2078589025 cites W2064143147 @default.
• W2078589025 cites W2072894233 @default.
• W2078589025 cites W2075063784 @default.
• W2078589025 cites W2082492557 @default.
• W2078589025 cites W2086383795 @default.
• W2078589025 cites W2096215200 @default.
• W2078589025 cites W2112841190 @default.
• W2078589025 cites W2132001331 @default.
• W2078589025 cites W2144945637 @default.
• W2078589025 cites W2326034505 @default.
• W2078589025 cites W2395188320 @default.
• W2078589025 cites W2478820444 @default.
• W2078589025 cites W2485381278 @default.
• W2078589025 cites W2503210287 @default.
• W2078589025 cites W355298964 @default.
• W2078589025 doi "https://doi.org/10.1016/s0040-1951(98)00011-0" @default.
• W2078589025 hasPublicationYear "1998" @default.
• W2078589025 type Work @default.
• W2078589025 sameAs 2078589025 @default.
• W2078589025 citedByCount "31" @default.
• W2078589025 countsByYear W20785890252012 @default.
• W2078589025 countsByYear W20785890252014 @default.
• W2078589025 countsByYear W20785890252015 @default.
• W2078589025 countsByYear W20785890252017 @default.
• W2078589025 countsByYear W20785890252019 @default.
• W2078589025 countsByYear W20785890252021 @default.
• W2078589025 crossrefType "journal-article" @default.
• W2078589025 hasAuthorship W2078589025A5004763780 @default.
• W2078589025 hasAuthorship W2078589025A5009966291 @default.
• W2078589025 hasAuthorship W2078589025A5038522902 @default.
• W2078589025 hasAuthorship W2078589025A5055780454 @default.
• W2078589025 hasAuthorship W2078589025A5064227339 @default.
• W2078589025 hasAuthorship W2078589025A5073974620 @default.
• W2078589025 hasConcept C115076146 @default.
• W2078589025 hasConcept C121704057 @default.
• W2078589025 hasConcept C127313418 @default.
• W2078589025 hasConcept C138885662 @default.
• W2078589025 hasConcept C151730666 @default.
• W2078589025 hasConcept C165205528 @default.
• W2078589025 hasConcept C2776698055 @default.
• W2078589025 hasConcept C2994012208 @default.
• W2078589025 hasConcept C38652104 @default.
• W2078589025 hasConcept C41008148 @default.
• W2078589025 hasConcept C41895202 @default.
• W2078589025 hasConceptScore W2078589025C115076146 @default.
• W2078589025 hasConceptScore W2078589025C121704057 @default.
• W2078589025 hasConceptScore W2078589025C127313418 @default.
• W2078589025 hasConceptScore W2078589025C138885662 @default.
• W2078589025 hasConceptScore W2078589025C151730666 @default.
• W2078589025 hasConceptScore W2078589025C165205528 @default.
• W2078589025 hasConceptScore W2078589025C2776698055 @default.
• W2078589025 hasConceptScore W2078589025C2994012208 @default.
• W2078589025 hasConceptScore W2078589025C38652104 @default.
• W2078589025 hasConceptScore W2078589025C41008148 @default.
• W2078589025 hasConceptScore W2078589025C41895202 @default.
• W2078589025 hasIssue "3-4" @default.
• W2078589025 hasLocation W20785890251 @default.
• W2078589025 hasOpenAccess W2078589025 @default.
• W2078589025 hasPrimaryLocation W20785890251 @default.
• W2078589025 hasRelatedWork W2010446848 @default.
• W2078589025 hasRelatedWork W2022784417 @default.
• W2078589025 hasRelatedWork W2053983673 @default.
• W2078589025 hasRelatedWork W2073444015 @default.
• W2078589025 hasRelatedWork W2366593754 @default.
• W2078589025 hasRelatedWork W2990054744 @default.
• W2078589025 hasRelatedWork W3121083000 @default.
• W2078589025 hasRelatedWork W3150138053 @default.
• W2078589025 hasRelatedWork W4226142241 @default.
• W2078589025 hasRelatedWork W818695416 @default.
• W2078589025 hasVolume "290" @default.
• W2078589025 isParatext "false" @default.
• W2078589025 isRetracted "false" @default.
• W2078589025 magId "2078589025" @default.
• W2078589025 workType "article" @default.