FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1984696687> ?p ?o ?g. }

• W1984696687 endingPage "242" @default.
• W1984696687 startingPage "229" @default.
• W1984696687 abstract "Granulite-facies gneisses of the late-Proterozoic Okiep Copper District of the Namaqua Province in South Africa preserve evidence of a range of anatectic melt features that reflect the initial stages of segregation and ascent of crustally derived magmas during high-grade metamorphism. These melt bodies include both in situ and sharply transgressive, subvertical, pipe-like bodies, that show vertical dimensions of several hundreds of metres and horizontal dimensions of tens to hundreds of metres. Migmatite bodies are spatially closely linked with narrow, upright zones characterized by intense high-strain fabrics, locally referred to as ‘steep structures’. They display a progressive textural development, from diktyonitic textures in in situ bodies, via schollen-and-raft textures to largely homogeneous intrusive granites that have migrated vertically for distances of several hundreds of metres or more. The intimate association of the migmatite bodies with the steep structures reflects strain-induced melt segregation, facilitated by increased permeabilities in these ductile deformation zones, and migration of melts into sites of strain incompatibility at the intersections between the regional subhorizontal gneissosity and the superimposed high-strain zones. Subsequent melt migration was focused along the network of subvertical structural anisotropies provided by the steep structures. Melt migration was controlled by a combination of buoyancy, shear-enhanced melt compaction during ongoing deformation, melt compaction due to the settling of wall-rock fragments from higher stratigraphiclevels and subordinate brittle fracturing. The unusual geometry of the steep structures and the intensely heterogeneous nature of the strain, and the absence of similar strain features and voluminous melt bodies elsewhere in the granulite-facies terrane, suggest a positive feed-back mechanism between melt generation and strain localization in steep structures. The structural development of the migmatite bodies illustrates that the efficiency of melt segregation and migration in a mid-crustal segment is dependent not only on the fertility of its lithologies, but also on its deformational style." @default.
• W1984696687 created "2016-06-24" @default.
• W1984696687 creator A5026677062 @default.
• W1984696687 creator A5035935613 @default.
• W1984696687 creator A5072792997 @default.
• W1984696687 creator A5080235116 @default.
• W1984696687 date "1998-02-01" @default.
• W1984696687 modified "2023-10-03" @default.
• W1984696687 title "The role of strain localization in the segregation and ascent of anatectic melts, Namaqualand, South Africa" @default.
• W1984696687 cites W1963649432 @default.
• W1984696687 cites W1966016940 @default.
• W1984696687 cites W1969654283 @default.
• W1984696687 cites W1971609705 @default.
• W1984696687 cites W1972645997 @default.
• W1984696687 cites W1978217098 @default.
• W1984696687 cites W1979355507 @default.
• W1984696687 cites W1983822564 @default.
• W1984696687 cites W1991101657 @default.
• W1984696687 cites W2004409367 @default.
• W1984696687 cites W2012366370 @default.
• W1984696687 cites W2023327969 @default.
• W1984696687 cites W2028299312 @default.
• W1984696687 cites W2029343011 @default.
• W1984696687 cites W2029884420 @default.
• W1984696687 cites W2037583736 @default.
• W1984696687 cites W2039039175 @default.
• W1984696687 cites W2039848826 @default.
• W1984696687 cites W2044455233 @default.
• W1984696687 cites W2052885790 @default.
• W1984696687 cites W2053470461 @default.
• W1984696687 cites W2065923829 @default.
• W1984696687 cites W2068538296 @default.
• W1984696687 cites W2075774577 @default.
• W1984696687 cites W2076576809 @default.
• W1984696687 cites W2078437864 @default.
• W1984696687 cites W2081831921 @default.
• W1984696687 cites W2083349594 @default.
• W1984696687 cites W2084980615 @default.
• W1984696687 cites W2088670614 @default.
• W1984696687 cites W2093150762 @default.
• W1984696687 cites W2094101024 @default.
• W1984696687 cites W2096317422 @default.
• W1984696687 cites W2098732737 @default.
• W1984696687 cites W2120027408 @default.
• W1984696687 cites W2127070160 @default.
• W1984696687 cites W2152984700 @default.
• W1984696687 cites W2314101103 @default.
• W1984696687 cites W2975847447 @default.
• W1984696687 cites W4256265735 @default.
• W1984696687 doi "https://doi.org/10.1016/s0191-8141(97)00081-3" @default.
• W1984696687 hasPublicationYear "1998" @default.
• W1984696687 type Work @default.
• W1984696687 sameAs 1984696687 @default.
• W1984696687 citedByCount "32" @default.
• W1984696687 countsByYear W19846966872012 @default.
• W1984696687 countsByYear W19846966872016 @default.
• W1984696687 countsByYear W19846966872018 @default.
• W1984696687 countsByYear W19846966872020 @default.
• W1984696687 countsByYear W19846966872021 @default.
• W1984696687 countsByYear W19846966872022 @default.
• W1984696687 crossrefType "journal-article" @default.
• W1984696687 hasAuthorship W1984696687A5026677062 @default.
• W1984696687 hasAuthorship W1984696687A5035935613 @default.
• W1984696687 hasAuthorship W1984696687A5072792997 @default.
• W1984696687 hasAuthorship W1984696687A5080235116 @default.
• W1984696687 hasConcept C109007969 @default.
• W1984696687 hasConcept C112764850 @default.
• W1984696687 hasConcept C114793014 @default.
• W1984696687 hasConcept C119073576 @default.
• W1984696687 hasConcept C127313418 @default.
• W1984696687 hasConcept C146588470 @default.
• W1984696687 hasConcept C165205528 @default.
• W1984696687 hasConcept C171701179 @default.
• W1984696687 hasConcept C17409809 @default.
• W1984696687 hasConcept C18142444 @default.
• W1984696687 hasConcept C23295444 @default.
• W1984696687 hasConcept C26687426 @default.
• W1984696687 hasConcept C2779557651 @default.
• W1984696687 hasConcept C5900021 @default.
• W1984696687 hasConcept C77928131 @default.
• W1984696687 hasConceptScore W1984696687C109007969 @default.
• W1984696687 hasConceptScore W1984696687C112764850 @default.
• W1984696687 hasConceptScore W1984696687C114793014 @default.
• W1984696687 hasConceptScore W1984696687C119073576 @default.
• W1984696687 hasConceptScore W1984696687C127313418 @default.
• W1984696687 hasConceptScore W1984696687C146588470 @default.
• W1984696687 hasConceptScore W1984696687C165205528 @default.
• W1984696687 hasConceptScore W1984696687C171701179 @default.
• W1984696687 hasConceptScore W1984696687C17409809 @default.
• W1984696687 hasConceptScore W1984696687C18142444 @default.
• W1984696687 hasConceptScore W1984696687C23295444 @default.
• W1984696687 hasConceptScore W1984696687C26687426 @default.
• W1984696687 hasConceptScore W1984696687C2779557651 @default.
• W1984696687 hasConceptScore W1984696687C5900021 @default.
• W1984696687 hasConceptScore W1984696687C77928131 @default.
• W1984696687 hasIssue "2-3" @default.
• W1984696687 hasLocation W19846966871 @default.
• W1984696687 hasOpenAccess W1984696687 @default.

• next