FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1500233042> ?p ?o ?g. }

• W1500233042 endingPage "542" @default.
• W1500233042 startingPage "531" @default.
• W1500233042 abstract "Using teleseismic waveform records from 363 broadband stations, we applied H–κ stacking of receiver functions to estimate crustal thickness ( H ) and average Vp/Vs ratio ( κ ) in the central and western North China Craton (NCC) and adjacent regions. Our results show that, except for thinning in the Cenozoic rifts and southern edge of the central NCC, H gradually thickens westward from ~30 km at the easternmost edge of the central NCC to >60 km near the northeastern margin of the Tibetan Plateau. κ exhibits complex variations, with locally high or low anomalies in the rifts, at the southern edge of the central NCC and at tectonic boundary zones. Low‐density uppermost mantle and distinct N–S differences are observed in the Ordos, suggesting typical cratonic crust. Thickened crust and complex variations in κ at the southwestern boundary of the Ordos may be related to the formation of the Palaeozoic Qilian Block and late uplift of the Tibetan Plateau. Thinned crust and locally high κ are observed in and near the Cenozoic rifts, suggesting complex crustal modifications that may have been caused by repeated reactivation at pre‐existing weak zones by successive thermal‐tectonic events. Thin crust and low κ are found at the southern edge of the central NCC, suggesting crustal modifications such as delamination, especially in the lower crust, which may be related to collision of the NCC and Yangtze Block. Copyright © 2012 John Wiley & Sons, Ltd." @default.
• W1500233042 created "2016-06-24" @default.
• W1500233042 creator A5037360393 @default.
• W1500233042 creator A5057362882 @default.
• W1500233042 creator A5083009984 @default.
• W1500233042 date "2012-12-17" @default.
• W1500233042 modified "2023-10-18" @default.
• W1500233042 title "Regional variations in crustal thickness and Vp/Vs ratio beneath the central–western North China Craton and adjacent regions" @default.
• W1500233042 cites W1565588354 @default.
• W1500233042 cites W1587624588 @default.
• W1500233042 cites W1966442211 @default.
• W1500233042 cites W1966700794 @default.
• W1500233042 cites W1967921001 @default.
• W1500233042 cites W1976467450 @default.
• W1500233042 cites W1978445071 @default.
• W1500233042 cites W1980985326 @default.
• W1500233042 cites W1988202950 @default.
• W1500233042 cites W1989945922 @default.
• W1500233042 cites W2001820253 @default.
• W1500233042 cites W2006146493 @default.
• W1500233042 cites W2006449183 @default.
• W1500233042 cites W2012512380 @default.
• W1500233042 cites W2024674080 @default.
• W1500233042 cites W2040177180 @default.
• W1500233042 cites W2040200942 @default.
• W1500233042 cites W2043003723 @default.
• W1500233042 cites W2046653975 @default.
• W1500233042 cites W2050309905 @default.
• W1500233042 cites W2051693684 @default.
• W1500233042 cites W2057266647 @default.
• W1500233042 cites W2061359484 @default.
• W1500233042 cites W2061416808 @default.
• W1500233042 cites W2077141827 @default.
• W1500233042 cites W2081696323 @default.
• W1500233042 cites W2083048657 @default.
• W1500233042 cites W2083266769 @default.
• W1500233042 cites W2094090764 @default.
• W1500233042 cites W2094194060 @default.
• W1500233042 cites W2094820155 @default.
• W1500233042 cites W2094963733 @default.
• W1500233042 cites W2097502986 @default.
• W1500233042 cites W2099550353 @default.
• W1500233042 cites W2129157266 @default.
• W1500233042 cites W2148550627 @default.
• W1500233042 cites W2149206681 @default.
• W1500233042 cites W2150092572 @default.
• W1500233042 cites W2152572862 @default.
• W1500233042 cites W2155858604 @default.
• W1500233042 cites W2166901676 @default.
• W1500233042 cites W2169278971 @default.
• W1500233042 cites W2336433437 @default.
• W1500233042 cites W2411308341 @default.
• W1500233042 cites W3092361928 @default.
• W1500233042 cites W4254422160 @default.
• W1500233042 doi "https://doi.org/10.1002/gj.2473" @default.
• W1500233042 hasPublicationYear "2012" @default.
• W1500233042 type Work @default.
• W1500233042 sameAs 1500233042 @default.
• W1500233042 citedByCount "12" @default.
• W1500233042 countsByYear W15002330422013 @default.
• W1500233042 countsByYear W15002330422015 @default.
• W1500233042 countsByYear W15002330422016 @default.
• W1500233042 countsByYear W15002330422018 @default.
• W1500233042 countsByYear W15002330422020 @default.
• W1500233042 countsByYear W15002330422021 @default.
• W1500233042 countsByYear W15002330422022 @default.
• W1500233042 crossrefType "journal-article" @default.
• W1500233042 hasAuthorship W1500233042A5037360393 @default.
• W1500233042 hasAuthorship W1500233042A5057362882 @default.
• W1500233042 hasAuthorship W1500233042A5083009984 @default.
• W1500233042 hasConcept C109007969 @default.
• W1500233042 hasConcept C127313418 @default.
• W1500233042 hasConcept C134306372 @default.
• W1500233042 hasConcept C147717901 @default.
• W1500233042 hasConcept C148447573 @default.
• W1500233042 hasConcept C151730666 @default.
• W1500233042 hasConcept C165205528 @default.
• W1500233042 hasConcept C16942324 @default.
• W1500233042 hasConcept C2776698055 @default.
• W1500233042 hasConcept C2780030769 @default.
• W1500233042 hasConcept C33923547 @default.
• W1500233042 hasConcept C50682988 @default.
• W1500233042 hasConcept C67236022 @default.
• W1500233042 hasConcept C73707237 @default.
• W1500233042 hasConcept C77928131 @default.
• W1500233042 hasConceptScore W1500233042C109007969 @default.
• W1500233042 hasConceptScore W1500233042C127313418 @default.
• W1500233042 hasConceptScore W1500233042C134306372 @default.
• W1500233042 hasConceptScore W1500233042C147717901 @default.
• W1500233042 hasConceptScore W1500233042C148447573 @default.
• W1500233042 hasConceptScore W1500233042C151730666 @default.
• W1500233042 hasConceptScore W1500233042C165205528 @default.
• W1500233042 hasConceptScore W1500233042C16942324 @default.
• W1500233042 hasConceptScore W1500233042C2776698055 @default.
• W1500233042 hasConceptScore W1500233042C2780030769 @default.
• W1500233042 hasConceptScore W1500233042C33923547 @default.
• W1500233042 hasConceptScore W1500233042C50682988 @default.
• W1500233042 hasConceptScore W1500233042C67236022 @default.

• next