FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2113594605> ?p ?o ?g. }

• W2113594605 endingPage "535" @default.
• W2113594605 startingPage "521" @default.
• W2113594605 abstract "Schists from the foothills of the Central Sierra Nevada contain one dominant matrix foliation and yet four phases of growth of both cordierite and andalusite porphyroblasts can be distinguished. These occurred early during four separate deformation events that formed successive steep and shallow foliations. A fifth deformation event pre-dates the growth of all porphyroblasts studied. The multiple phases of porphyroblast growth allow correlation of structures across and along the region. A repeated pattern of deformation, in terms of the curvature of earlier foliations against the overprinting one, allows samples containing porphyroblasts with simpler inclusion trail geometries to be interpreted with confidence. The large-scale fold structures in this region formed before or during the second of the five deformation events recorded by the porphyroblasts. However, the matrix foliation is predominantly a product of the fourth deformation, which has commonly reactivated or re-used older foliations, and is dominated by east-side-up shear. The intervening third deformation produced locally intense foliations and was accompanied by top-to-the-east shear. The very weak fifth deformation produced weak crenulations with subhorizontal axial planes and was coaxial. Multiple phases of episodic but synchronous growth of cordierite and andalusite were produced by the KFMASH univariant equilibrium Ms+Chl+Qtz=And+Crd+Bt+H2O. The rocks crossed this reaction at a pressure just below the intersection with the KFMASH divariant equilibrium Ms+Chl+Qtz=Crd+Bt+H2O; the latter being overstepped in favour of the former as there is no evidence for cordierite growth prior to andalusite in these rocks. Subsequent multiple episodes of synchronous growth of cordierite and andalusite indicate that the possible variation in P–T during subsequent deformations was not large. This requires the high-amplitude macroscopic fold to form prior to porphyroblast growth and then be simply tightened and modified by the younger deformations." @default.
• W2113594605 created "2016-06-24" @default.
• W2113594605 creator A5000382536 @default.
• W2113594605 creator A5042781128 @default.
• W2113594605 date "1999-09-01" @default.
• W2113594605 modified "2023-10-13" @default.
• W2113594605 title "Complex microstructures preserved in rocks with a simple matrix: significance for deformation and metamorphic processes" @default.
• W2113594605 cites W1974148086 @default.
• W2113594605 cites W1997512060 @default.
• W2113594605 cites W2005024530 @default.
• W2113594605 cites W2006667472 @default.
• W2113594605 cites W2013455995 @default.
• W2113594605 cites W2018590776 @default.
• W2113594605 cites W2025003938 @default.
• W2113594605 cites W2026046120 @default.
• W2113594605 cites W2031836336 @default.
• W2113594605 cites W2046713291 @default.
• W2113594605 cites W2051300481 @default.
• W2113594605 cites W2054337691 @default.
• W2113594605 cites W2070062931 @default.
• W2113594605 cites W2075685982 @default.
• W2113594605 cites W2079121796 @default.
• W2113594605 cites W2081886512 @default.
• W2113594605 cites W2093788562 @default.
• W2113594605 cites W2123453243 @default.
• W2113594605 cites W2137627251 @default.
• W2113594605 cites W2319640931 @default.
• W2113594605 cites W2586518786 @default.
• W2113594605 doi "https://doi.org/10.1046/j.1525-1314.1999.00214.x" @default.
• W2113594605 hasPublicationYear "1999" @default.
• W2113594605 type Work @default.
• W2113594605 sameAs 2113594605 @default.
• W2113594605 citedByCount "32" @default.
• W2113594605 countsByYear W21135946052017 @default.
• W2113594605 countsByYear W21135946052018 @default.
• W2113594605 countsByYear W21135946052019 @default.
• W2113594605 crossrefType "journal-article" @default.
• W2113594605 hasAuthorship W2113594605A5000382536 @default.
• W2113594605 hasAuthorship W2113594605A5042781128 @default.
• W2113594605 hasConcept C101082671 @default.
• W2113594605 hasConcept C101139013 @default.
• W2113594605 hasConcept C106487976 @default.
• W2113594605 hasConcept C111368507 @default.
• W2113594605 hasConcept C112764850 @default.
• W2113594605 hasConcept C123283553 @default.
• W2113594605 hasConcept C127313418 @default.
• W2113594605 hasConcept C134132462 @default.
• W2113594605 hasConcept C159985019 @default.
• W2113594605 hasConcept C165205528 @default.
• W2113594605 hasConcept C168425004 @default.
• W2113594605 hasConcept C17409809 @default.
• W2113594605 hasConcept C192562407 @default.
• W2113594605 hasConcept C199289684 @default.
• W2113594605 hasConcept C204366326 @default.
• W2113594605 hasConcept C205539056 @default.
• W2113594605 hasConcept C23295444 @default.
• W2113594605 hasConcept C26687426 @default.
• W2113594605 hasConcept C2776813687 @default.
• W2113594605 hasConcept C2777545297 @default.
• W2113594605 hasConcept C2778660078 @default.
• W2113594605 hasConcept C5900021 @default.
• W2113594605 hasConcept C77928131 @default.
• W2113594605 hasConcept C87976508 @default.
• W2113594605 hasConcept C96035792 @default.
• W2113594605 hasConceptScore W2113594605C101082671 @default.
• W2113594605 hasConceptScore W2113594605C101139013 @default.
• W2113594605 hasConceptScore W2113594605C106487976 @default.
• W2113594605 hasConceptScore W2113594605C111368507 @default.
• W2113594605 hasConceptScore W2113594605C112764850 @default.
• W2113594605 hasConceptScore W2113594605C123283553 @default.
• W2113594605 hasConceptScore W2113594605C127313418 @default.
• W2113594605 hasConceptScore W2113594605C134132462 @default.
• W2113594605 hasConceptScore W2113594605C159985019 @default.
• W2113594605 hasConceptScore W2113594605C165205528 @default.
• W2113594605 hasConceptScore W2113594605C168425004 @default.
• W2113594605 hasConceptScore W2113594605C17409809 @default.
• W2113594605 hasConceptScore W2113594605C192562407 @default.
• W2113594605 hasConceptScore W2113594605C199289684 @default.
• W2113594605 hasConceptScore W2113594605C204366326 @default.
• W2113594605 hasConceptScore W2113594605C205539056 @default.
• W2113594605 hasConceptScore W2113594605C23295444 @default.
• W2113594605 hasConceptScore W2113594605C26687426 @default.
• W2113594605 hasConceptScore W2113594605C2776813687 @default.
• W2113594605 hasConceptScore W2113594605C2777545297 @default.
• W2113594605 hasConceptScore W2113594605C2778660078 @default.
• W2113594605 hasConceptScore W2113594605C5900021 @default.
• W2113594605 hasConceptScore W2113594605C77928131 @default.
• W2113594605 hasConceptScore W2113594605C87976508 @default.
• W2113594605 hasConceptScore W2113594605C96035792 @default.
• W2113594605 hasIssue "5" @default.
• W2113594605 hasLocation W21135946051 @default.
• W2113594605 hasOpenAccess W2113594605 @default.
• W2113594605 hasPrimaryLocation W21135946051 @default.
• W2113594605 hasRelatedWork W1509480018 @default.
• W2113594605 hasRelatedWork W1965938127 @default.
• W2113594605 hasRelatedWork W1966376840 @default.
• W2113594605 hasRelatedWork W2045389041 @default.
• W2113594605 hasRelatedWork W2047419731 @default.

• next