FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2080762191> ?p ?o ?g. }

• W2080762191 endingPage "1059" @default.
• W2080762191 startingPage "1049" @default.
• W2080762191 abstract "Magnetotelluric (MT) sounding shows that the layers with low electrical resistivity less than 10 Ωm, much smaller than the average resistivity of crust in tectonically stable regions, exist extensively in the mid-lower crust of the Tibetan Plateau. Analysis suggests that these layers of enhanced conductance are not caused by metallic minerals, graphite, or saltine fluids, instead very likely formed by partial melt of rocks or a combination of partial melt and saltine fluids. The formation of these conductive layers in the crust is closely associated with the dynamic process of plate movement. Highly conductive layers in the crust of the Tibetan Plateau might be the electrical trace of the subduction of the India plate beneath Asia, during which frictional heating led to partial melt and dehydration at high pressure and high temperature. It may also be related with the upwelling of mantle source matters caused by lithosphere delamination. That the east-west trending high conductivity structures are continuously distributed along the major suture zones within the plateau might be the evidence for eastward channel flow of lower crust matter beneath the Tibetan Plateau. Among these suture zones, the Bangong-Nujiang suture zone is the most important channel for the transportation of lower crust material." @default.
• W2080762191 created "2016-06-24" @default.
• W2080762191 creator A5051434566 @default.
• W2080762191 creator A5052715795 @default.
• W2080762191 creator A5057195398 @default.
• W2080762191 creator A5079631711 @default.
• W2080762191 creator A5088181315 @default.
• W2080762191 creator A5088186198 @default.
• W2080762191 date "2010-11-01" @default.
• W2080762191 modified "2023-10-01" @default.
• W2080762191 title "On Genesis of Highly Conductive Layers in the Crust of the Tibetan Plateau and Its Dynamic Implications: Evidence from Magnetotelluric Sounding Data" @default.
• W2080762191 cites W1539332683 @default.
• W2080762191 cites W1570610859 @default.
• W2080762191 cites W1968253241 @default.
• W2080762191 cites W1980603372 @default.
• W2080762191 cites W2006758606 @default.
• W2080762191 cites W2007751710 @default.
• W2080762191 cites W2008008578 @default.
• W2080762191 cites W2010919613 @default.
• W2080762191 cites W2015925618 @default.
• W2080762191 cites W2040403706 @default.
• W2080762191 cites W2040923331 @default.
• W2080762191 cites W2062737820 @default.
• W2080762191 cites W2070311757 @default.
• W2080762191 cites W2093148123 @default.
• W2080762191 cites W2095646703 @default.
• W2080762191 cites W2144583290 @default.
• W2080762191 cites W2168607185 @default.
• W2080762191 cites W2304874705 @default.
• W2080762191 cites W2318148662 @default.
• W2080762191 doi "https://doi.org/10.1002/cjg2.1575" @default.
• W2080762191 hasPublicationYear "2010" @default.
• W2080762191 type Work @default.
• W2080762191 sameAs 2080762191 @default.
• W2080762191 citedByCount "0" @default.
• W2080762191 crossrefType "journal-article" @default.
• W2080762191 hasAuthorship W2080762191A5051434566 @default.
• W2080762191 hasAuthorship W2080762191A5052715795 @default.
• W2080762191 hasAuthorship W2080762191A5057195398 @default.
• W2080762191 hasAuthorship W2080762191A5079631711 @default.
• W2080762191 hasAuthorship W2080762191A5088181315 @default.
• W2080762191 hasAuthorship W2080762191A5088186198 @default.
• W2080762191 hasConcept C105702510 @default.
• W2080762191 hasConcept C111368507 @default.
• W2080762191 hasConcept C112313211 @default.
• W2080762191 hasConcept C119599485 @default.
• W2080762191 hasConcept C127313418 @default.
• W2080762191 hasConcept C127413603 @default.
• W2080762191 hasConcept C134306372 @default.
• W2080762191 hasConcept C149348798 @default.
• W2080762191 hasConcept C150999391 @default.
• W2080762191 hasConcept C165205528 @default.
• W2080762191 hasConcept C16942324 @default.
• W2080762191 hasConcept C17409809 @default.
• W2080762191 hasConcept C2776698055 @default.
• W2080762191 hasConcept C2777327002 @default.
• W2080762191 hasConcept C2780030769 @default.
• W2080762191 hasConcept C33923547 @default.
• W2080762191 hasConcept C58097730 @default.
• W2080762191 hasConcept C5900021 @default.
• W2080762191 hasConcept C67236022 @default.
• W2080762191 hasConcept C69990965 @default.
• W2080762191 hasConcept C71924100 @default.
• W2080762191 hasConcept C77928131 @default.
• W2080762191 hasConcept C79572550 @default.
• W2080762191 hasConcept C8058405 @default.
• W2080762191 hasConceptScore W2080762191C105702510 @default.
• W2080762191 hasConceptScore W2080762191C111368507 @default.
• W2080762191 hasConceptScore W2080762191C112313211 @default.
• W2080762191 hasConceptScore W2080762191C119599485 @default.
• W2080762191 hasConceptScore W2080762191C127313418 @default.
• W2080762191 hasConceptScore W2080762191C127413603 @default.
• W2080762191 hasConceptScore W2080762191C134306372 @default.
• W2080762191 hasConceptScore W2080762191C149348798 @default.
• W2080762191 hasConceptScore W2080762191C150999391 @default.
• W2080762191 hasConceptScore W2080762191C165205528 @default.
• W2080762191 hasConceptScore W2080762191C16942324 @default.
• W2080762191 hasConceptScore W2080762191C17409809 @default.
• W2080762191 hasConceptScore W2080762191C2776698055 @default.
• W2080762191 hasConceptScore W2080762191C2777327002 @default.
• W2080762191 hasConceptScore W2080762191C2780030769 @default.
• W2080762191 hasConceptScore W2080762191C33923547 @default.
• W2080762191 hasConceptScore W2080762191C58097730 @default.
• W2080762191 hasConceptScore W2080762191C5900021 @default.
• W2080762191 hasConceptScore W2080762191C67236022 @default.
• W2080762191 hasConceptScore W2080762191C69990965 @default.
• W2080762191 hasConceptScore W2080762191C71924100 @default.
• W2080762191 hasConceptScore W2080762191C77928131 @default.
• W2080762191 hasConceptScore W2080762191C79572550 @default.
• W2080762191 hasConceptScore W2080762191C8058405 @default.
• W2080762191 hasIssue "6" @default.
• W2080762191 hasLocation W20807621911 @default.
• W2080762191 hasOpenAccess W2080762191 @default.
• W2080762191 hasPrimaryLocation W20807621911 @default.
• W2080762191 hasRelatedWork W1527325679 @default.
• W2080762191 hasRelatedWork W2080762191 @default.
• W2080762191 hasRelatedWork W2166894955 @default.
• W2080762191 hasRelatedWork W2369094135 @default.

• next