FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2050832273> ?p ?o ?g. }

• W2050832273 endingPage "238" @default.
• W2050832273 startingPage "213" @default.
• W2050832273 abstract "Abstract The evolution of the Himalaya and the tectonics of neighbouring regions are generally believed to be due to continent-to-continent collision of the Eurasian and the Indian plates. During the last decade, many new data have been obtained and examined and a suite of models has been developed to explain the evolution of the Himalaya and the neighbouring regions. These models could broadly be classified into three categories. The subdivision of the Himalaya into five main structural units is now well accepted. A tectogenetic diagram of the Himalaya is briefly discussed. Ophiolites are reported to occur all along the Indus-Tsangpo Suture zone. Results of geochemical analysis of an ophiolite sequence from Dras in Kashmir Himalaya are presented. Surface wave dispersion and attenuation investigations have revealed the crustal and upper mantle structure below the Himalaya and Tibet plateau. The finding of low-velocity layers is consistent with the concept that horizontal compression has been responsible for creating these weak zones and the inferred elevated temperatures in the vicinity of the Moho discontinuity below Tibet. Earthquake focal-mechanism solutions and interpretation of Landsat imagery indicate that convergence of the Indian plate with Eurasia continues and is accommodated partly by crustal shortening and partly by lateral mass movement at the northwest and the northeast margins of the Indian plate. Palaeomagnetic data from the Himalaya belt and central Asia can be interpreted in support of Molnar and Tapponnier's model of continental collision." @default.
• W2050832273 created "2016-06-24" @default.
• W2050832273 creator A5035092011 @default.
• W2050832273 creator A5091240427 @default.
• W2050832273 creator A5091333455 @default.
• W2050832273 date "1982-01-01" @default.
• W2050832273 modified "2023-10-18" @default.
• W2050832273 title "Continental collision tectonics: Evidence from the Himalaya and the neighbouring regions" @default.
• W2050832273 cites W1968884284 @default.
• W2050832273 cites W1981713949 @default.
• W2050832273 cites W1981846615 @default.
• W2050832273 cites W1982293041 @default.
• W2050832273 cites W1982340989 @default.
• W2050832273 cites W1983530480 @default.
• W2050832273 cites W1985495015 @default.
• W2050832273 cites W1995083138 @default.
• W2050832273 cites W1997667374 @default.
• W2050832273 cites W2002325302 @default.
• W2050832273 cites W2006917661 @default.
• W2050832273 cites W2009716625 @default.
• W2050832273 cites W2022655390 @default.
• W2050832273 cites W2026301874 @default.
• W2050832273 cites W2027437929 @default.
• W2050832273 cites W2032490186 @default.
• W2050832273 cites W2036015936 @default.
• W2050832273 cites W2037408384 @default.
• W2050832273 cites W2043749257 @default.
• W2050832273 cites W2044534671 @default.
• W2050832273 cites W2047582516 @default.
• W2050832273 cites W2048727405 @default.
• W2050832273 cites W2053211094 @default.
• W2050832273 cites W2062970186 @default.
• W2050832273 cites W2064663101 @default.
• W2050832273 cites W2076733469 @default.
• W2050832273 cites W2081248227 @default.
• W2050832273 cites W2082085332 @default.
• W2050832273 cites W2082815954 @default.
• W2050832273 cites W2087272215 @default.
• W2050832273 cites W2089783228 @default.
• W2050832273 cites W2091894488 @default.
• W2050832273 cites W2092076980 @default.
• W2050832273 cites W2093671367 @default.
• W2050832273 cites W2099142396 @default.
• W2050832273 cites W2111555634 @default.
• W2050832273 cites W2112931403 @default.
• W2050832273 cites W2120560912 @default.
• W2050832273 cites W2161013684 @default.
• W2050832273 cites W52346890 @default.
• W2050832273 doi "https://doi.org/10.1016/0040-1951(82)90130-5" @default.
• W2050832273 hasPublicationYear "1982" @default.
• W2050832273 type Work @default.
• W2050832273 sameAs 2050832273 @default.
• W2050832273 citedByCount "14" @default.
• W2050832273 countsByYear W20508322732023 @default.
• W2050832273 crossrefType "journal-article" @default.
• W2050832273 hasAuthorship W2050832273A5035092011 @default.
• W2050832273 hasAuthorship W2050832273A5091240427 @default.
• W2050832273 hasAuthorship W2050832273A5091333455 @default.
• W2050832273 hasConcept C121704057 @default.
• W2050832273 hasConcept C127313418 @default.
• W2050832273 hasConcept C151730666 @default.
• W2050832273 hasConcept C165205528 @default.
• W2050832273 hasConcept C16942324 @default.
• W2050832273 hasConcept C192367031 @default.
• W2050832273 hasConcept C38652104 @default.
• W2050832273 hasConcept C41008148 @default.
• W2050832273 hasConcept C75643213 @default.
• W2050832273 hasConcept C77928131 @default.
• W2050832273 hasConceptScore W2050832273C121704057 @default.
• W2050832273 hasConceptScore W2050832273C127313418 @default.
• W2050832273 hasConceptScore W2050832273C151730666 @default.
• W2050832273 hasConceptScore W2050832273C165205528 @default.
• W2050832273 hasConceptScore W2050832273C16942324 @default.
• W2050832273 hasConceptScore W2050832273C192367031 @default.
• W2050832273 hasConceptScore W2050832273C38652104 @default.
• W2050832273 hasConceptScore W2050832273C41008148 @default.
• W2050832273 hasConceptScore W2050832273C75643213 @default.
• W2050832273 hasConceptScore W2050832273C77928131 @default.
• W2050832273 hasIssue "3-4" @default.
• W2050832273 hasLocation W20508322731 @default.
• W2050832273 hasOpenAccess W2050832273 @default.
• W2050832273 hasPrimaryLocation W20508322731 @default.
• W2050832273 hasRelatedWork W2089579066 @default.
• W2050832273 hasRelatedWork W2103796536 @default.
• W2050832273 hasRelatedWork W2124941805 @default.
• W2050832273 hasRelatedWork W2342346054 @default.
• W2050832273 hasRelatedWork W2351741731 @default.
• W2050832273 hasRelatedWork W2365440485 @default.
• W2050832273 hasRelatedWork W2368896742 @default.
• W2050832273 hasRelatedWork W2892711175 @default.
• W2050832273 hasRelatedWork W2995356210 @default.
• W2050832273 hasRelatedWork W4385198985 @default.
• W2050832273 hasVolume "81" @default.
• W2050832273 isParatext "false" @default.
• W2050832273 isRetracted "false" @default.
• W2050832273 magId "2050832273" @default.
• W2050832273 workType "article" @default.