FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2471296747> ?p ?o ?g. }

• W2471296747 endingPage "1040" @default.
• W2471296747 startingPage "1033" @default.
• W2471296747 abstract "Phulad Shear Zone (PSZ) of Delhi Fold Belt in Rajasthan is a northeasterly striking ductile shear zone with a well developed mylonitic foliation (035/70E) and a downdip stretching lineation. The deformation in the PSZ has developed in a transpressional regime with thrusting sense of movement. The northeastern unit, i.e., the hanging wall contains a variety of rocks namely calc-silicates, pelites and amphibolites and the southwestern unit, i.e., the footwall unit contains only granitic rocks. Systematic investigation of the granites of the southwestern unit indicate a gradual change in the intensity of deformation from a distance of about 1 km west of the shear zone to the shear zone proper. The granite changes from weakly deformed granite to a mylonite/ultramylonite as we proceed towards the PSZ. The weakly deformed granite shows a crude foliation with the same attitude of mylonitic foliation of the PSZ. Microscopic study reveals the incipient development of C and S fabric with angle between C and S varying from 15 ∘ to 24 ∘. The small angle between the C and S fabric in the least deformed granite variety indicates that the deformation has strong pure shear component. At a distance of about 1 m away from the PSZ, there is abrupt change in the intensity of deformation. The granite becomes intensely foliated with a strong downdip lineation and the rock becomes a true mylonite. In mesoscopic scale, the granite shows stretched porphyroclasts in both XZ and YZ sections indicating a flattening type of deformation. The angle between the C and S fabric is further reduced and finally becomes nearly parallel. In most places, S fabric is gradually replaced by C fabric. Calculation of sectional kinematic vorticity number ( W n) from the protomylonitic and mylonite/ultramylonite granites varies from 0.3 ± 0.03 to 0.55 ± 0.04 indicating a strong component of pure shear. The similarity of the geometry of structures in the PSZ and the granites demonstrates that the deformation of the two units is broadly synchronous and the deformation in both the units is transpressional." @default.
• W2471296747 created "2016-07-22" @default.
• W2471296747 creator A5014077658 @default.
• W2471296747 creator A5025082018 @default.
• W2471296747 creator A5042237330 @default.
• W2471296747 creator A5072430957 @default.
• W2471296747 date "2016-07-01" @default.
• W2471296747 modified "2023-10-18" @default.
• W2471296747 title "Deformation of footwall rock of Phulad Shear Zone, Rajasthan: Evidence of transpressional shear zone" @default.
• W2471296747 cites W1964652436 @default.
• W2471296747 cites W1968692348 @default.
• W2471296747 cites W2000260511 @default.
• W2471296747 cites W2010362600 @default.
• W2471296747 cites W2020640770 @default.
• W2471296747 cites W2021766757 @default.
• W2471296747 cites W2023430719 @default.
• W2471296747 cites W2028473005 @default.
• W2471296747 cites W2059618046 @default.
• W2471296747 cites W2069801365 @default.
• W2471296747 cites W2071610076 @default.
• W2471296747 cites W2089908125 @default.
• W2471296747 cites W2150418263 @default.
• W2471296747 cites W2172251469 @default.
• W2471296747 cites W2298012029 @default.
• W2471296747 cites W29687769 @default.
• W2471296747 cites W4301156473 @default.
• W2471296747 doi "https://doi.org/10.1007/s12040-016-0713-y" @default.
• W2471296747 hasPublicationYear "2016" @default.
• W2471296747 type Work @default.
• W2471296747 sameAs 2471296747 @default.
• W2471296747 citedByCount "10" @default.
• W2471296747 countsByYear W24712967472017 @default.
• W2471296747 countsByYear W24712967472019 @default.
• W2471296747 countsByYear W24712967472020 @default.
• W2471296747 countsByYear W24712967472021 @default.
• W2471296747 countsByYear W24712967472022 @default.
• W2471296747 countsByYear W24712967472023 @default.
• W2471296747 crossrefType "journal-article" @default.
• W2471296747 hasAuthorship W2471296747A5014077658 @default.
• W2471296747 hasAuthorship W2471296747A5025082018 @default.
• W2471296747 hasAuthorship W2471296747A5042237330 @default.
• W2471296747 hasAuthorship W2471296747A5072430957 @default.
• W2471296747 hasBestOaLocation W24712967472 @default.
• W2471296747 hasConcept C101082671 @default.
• W2471296747 hasConcept C111368507 @default.
• W2471296747 hasConcept C127313418 @default.
• W2471296747 hasConcept C165205528 @default.
• W2471296747 hasConcept C17409809 @default.
• W2471296747 hasConcept C197737763 @default.
• W2471296747 hasConcept C199289684 @default.
• W2471296747 hasConcept C204366326 @default.
• W2471296747 hasConcept C23295444 @default.
• W2471296747 hasConcept C5900021 @default.
• W2471296747 hasConcept C77928131 @default.
• W2471296747 hasConcept C96035792 @default.
• W2471296747 hasConcept C98742433 @default.
• W2471296747 hasConceptScore W2471296747C101082671 @default.
• W2471296747 hasConceptScore W2471296747C111368507 @default.
• W2471296747 hasConceptScore W2471296747C127313418 @default.
• W2471296747 hasConceptScore W2471296747C165205528 @default.
• W2471296747 hasConceptScore W2471296747C17409809 @default.
• W2471296747 hasConceptScore W2471296747C197737763 @default.
• W2471296747 hasConceptScore W2471296747C199289684 @default.
• W2471296747 hasConceptScore W2471296747C204366326 @default.
• W2471296747 hasConceptScore W2471296747C23295444 @default.
• W2471296747 hasConceptScore W2471296747C5900021 @default.
• W2471296747 hasConceptScore W2471296747C77928131 @default.
• W2471296747 hasConceptScore W2471296747C96035792 @default.
• W2471296747 hasConceptScore W2471296747C98742433 @default.
• W2471296747 hasFunder F4320326716 @default.
• W2471296747 hasIssue "5" @default.
• W2471296747 hasLocation W24712967471 @default.
• W2471296747 hasLocation W24712967472 @default.
• W2471296747 hasOpenAccess W2471296747 @default.
• W2471296747 hasPrimaryLocation W24712967471 @default.
• W2471296747 hasRelatedWork W161046653 @default.
• W2471296747 hasRelatedWork W166665929 @default.
• W2471296747 hasRelatedWork W17616255 @default.
• W2471296747 hasRelatedWork W1996923439 @default.
• W2471296747 hasRelatedWork W2034324780 @default.
• W2471296747 hasRelatedWork W2057089776 @default.
• W2471296747 hasRelatedWork W2272975080 @default.
• W2471296747 hasRelatedWork W24059577 @default.
• W2471296747 hasRelatedWork W2589020515 @default.
• W2471296747 hasRelatedWork W3046050329 @default.
• W2471296747 hasVolume "125" @default.
• W2471296747 isParatext "false" @default.
• W2471296747 isRetracted "false" @default.
• W2471296747 magId "2471296747" @default.
• W2471296747 workType "article" @default.