FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1583648055> ?p ?o ?g. }

• W1583648055 abstract "As a long-term geological process with widespread influence, destruction of the North China Craton (NCC) displays many important geological phenomena and attracts interest of many domestic and overseas researchers engaged in geology, geochemistry and geophysics, etc. The NCC has its own attributes of occurrence and development. Its destruction may have connections with the activities of YYOB and QDOB respectively, distributed in the north and the south, as well as with the subduction between Indian plate and Pacific plate. Even though the inhomogeneity of the destruction process becomes prominent in terms of time, space and destruction intensity, significant disputes still exist on several specific problems. The peak period of NCC destruction was in late Jurassic-early Cretaceous. However, there are various opinions concerning the determination of beginning stage, e. g. 1) late Triassic (Menzies et al., 1998; Gao et al., 2002; Lu Fengxiang et al., 2000; Yang Jinhui et al., 2009); 2) late Mesozoic (Deng Jinfu et al.,1994; Wu Fuyuan et al., 1999; Zhai Mingguo et al., 2003; Lu Fengxiang et al.,2006); 3) Cenozoic (Menzies et al., 1993; Griffin et al., 1998; Xu, 2001) and Meso-Cenozoic (Xu Wenliang et al., 2000); or even in 4) late Paleozoic (Xu Yigang et al., 2009; Li Hongyan et al., 2009). The range of NCC destruction is in the east of the gravity gradient zone of (from Daxing’anling Mountains to) Taihangshan Mountains (Xu Yigang et al., 2006) , according to other opinions, or already had moved westward to nearby of Luliangshan Mountain (Ren Zhanli et al., 2005; Xiao Yuanyuan et al., 2007) around the Shanxi province as transitional or conversional area (Xing Zuoyun et al., 2006). The destruction intensity is getting gradually stronger from west to east, extremely severe in the east (Wei Wenbo et al., 2008), stable in the western Ordos area which remains as typical craton without disturbance in its deep layer by NCC destruction (Qiu Ruizhao et al., 2004; Jia Shixu et al., 2005). NCC destruction, as a geological process, was a kind of gradually" @default.
• W1583648055 created "2016-06-24" @default.
• W1583648055 creator A5006079292 @default.
• W1583648055 creator A5030770758 @default.
• W1583648055 creator A5037773587 @default.
• W1583648055 creator A5048001026 @default.
• W1583648055 creator A5074642572 @default.
• W1583648055 date "2011-02-28" @default.
• W1583648055 modified "2023-09-26" @default.
• W1583648055 title "Proto-Basin Types of North China Craton (NCC) in Late Triassic and Its Implication for Regional Tectonics of Initial Craton Destruction" @default.
• W1583648055 cites W1034423882 @default.
• W1583648055 cites W1490712700 @default.
• W1583648055 cites W1585382097 @default.
• W1583648055 cites W1587624588 @default.
• W1583648055 cites W1879935531 @default.
• W1583648055 cites W1979172119 @default.
• W1583648055 cites W2006713945 @default.
• W1583648055 cites W2050309905 @default.
• W1583648055 cites W2052280465 @default.
• W1583648055 cites W2071372910 @default.
• W1583648055 cites W2094820155 @default.
• W1583648055 cites W2149183324 @default.
• W1583648055 cites W2169278971 @default.
• W1583648055 cites W2347984454 @default.
• W1583648055 cites W2348127444 @default.
• W1583648055 cites W2348347326 @default.
• W1583648055 cites W2349697457 @default.
• W1583648055 cites W2351759767 @default.
• W1583648055 cites W2353383300 @default.
• W1583648055 cites W2353630526 @default.
• W1583648055 cites W2354149513 @default.
• W1583648055 cites W2356455578 @default.
• W1583648055 cites W2356473757 @default.
• W1583648055 cites W2356496139 @default.
• W1583648055 cites W2357078607 @default.
• W1583648055 cites W2361092424 @default.
• W1583648055 cites W2361430078 @default.
• W1583648055 cites W2362046146 @default.
• W1583648055 cites W2362985308 @default.
• W1583648055 cites W2363097693 @default.
• W1583648055 cites W2363782287 @default.
• W1583648055 cites W2363959016 @default.
• W1583648055 cites W2366714107 @default.
• W1583648055 cites W2366919149 @default.
• W1583648055 cites W2367674274 @default.
• W1583648055 cites W2368415085 @default.
• W1583648055 cites W2371549651 @default.
• W1583648055 cites W2372560933 @default.
• W1583648055 cites W2376133542 @default.
• W1583648055 cites W2378883427 @default.
• W1583648055 cites W2381436725 @default.
• W1583648055 cites W2382639954 @default.
• W1583648055 cites W2383114644 @default.
• W1583648055 cites W2385749819 @default.
• W1583648055 cites W2386392403 @default.
• W1583648055 cites W2389309934 @default.
• W1583648055 cites W2390714724 @default.
• W1583648055 cites W2393282915 @default.
• W1583648055 cites W2394065776 @default.
• W1583648055 cites W2411308341 @default.
• W1583648055 cites W2977433327 @default.
• W1583648055 cites W3147531084 @default.
• W1583648055 cites W585197870 @default.
• W1583648055 cites W601003954 @default.
• W1583648055 cites W987797604 @default.
• W1583648055 doi "https://doi.org/10.5772/14061" @default.
• W1583648055 hasPublicationYear "2011" @default.
• W1583648055 type Work @default.
• W1583648055 sameAs 1583648055 @default.
• W1583648055 citedByCount "0" @default.
• W1583648055 crossrefType "book-chapter" @default.
• W1583648055 hasAuthorship W1583648055A5006079292 @default.
• W1583648055 hasAuthorship W1583648055A5030770758 @default.
• W1583648055 hasAuthorship W1583648055A5037773587 @default.
• W1583648055 hasAuthorship W1583648055A5048001026 @default.
• W1583648055 hasAuthorship W1583648055A5074642572 @default.
• W1583648055 hasBestOaLocation W15836480551 @default.
• W1583648055 hasConcept C109007969 @default.
• W1583648055 hasConcept C127313418 @default.
• W1583648055 hasConcept C147717901 @default.
• W1583648055 hasConcept C151730666 @default.
• W1583648055 hasConcept C166957645 @default.
• W1583648055 hasConcept C17409809 @default.
• W1583648055 hasConcept C191935318 @default.
• W1583648055 hasConcept C1965285 @default.
• W1583648055 hasConcept C205649164 @default.
• W1583648055 hasConcept C77928131 @default.
• W1583648055 hasConceptScore W1583648055C109007969 @default.
• W1583648055 hasConceptScore W1583648055C127313418 @default.
• W1583648055 hasConceptScore W1583648055C147717901 @default.
• W1583648055 hasConceptScore W1583648055C151730666 @default.
• W1583648055 hasConceptScore W1583648055C166957645 @default.
• W1583648055 hasConceptScore W1583648055C17409809 @default.
• W1583648055 hasConceptScore W1583648055C191935318 @default.
• W1583648055 hasConceptScore W1583648055C1965285 @default.
• W1583648055 hasConceptScore W1583648055C205649164 @default.
• W1583648055 hasConceptScore W1583648055C77928131 @default.
• W1583648055 hasLocation W15836480551 @default.
• W1583648055 hasOpenAccess W1583648055 @default.
• W1583648055 hasPrimaryLocation W15836480551 @default.

• next