FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2165200576> ?p ?o ?g. }

• W2165200576 endingPage "211" @default.
• W2165200576 startingPage "195" @default.
• W2165200576 abstract "Abstract Dissolution of quartz and the recryst-allization and re-equilibration of phyllosilicates produce the dark anastomosing seams that dominate microstructures of tectonic melange which occur in a low-grade, imbricated and multiply deformed, mid-Palaeozoic, intracra-tonic fiysch sequence in northeastern Australia. Seams are composed of very closely spaced or coalesced cleavage lamellae, which are very thin layers of extremely fine-grained phyllosilicates. Cleavage seams enclose lenses of silt-stone or greywacke, which formerly occurred in continuous sedimentary layers, indicating extremely heterogeneous and disruptive deformation. Microphacoids enclosed by cleavage seams have subtle shape asymmetries analogous to those of porphyroclasts. Phyllosilicate-preferred orientations within microphacoids commonly lie at a low angle to enclosing seams, and asymmetric relationships occur within seams. The shape and fabric asymmetries appear to be constant, and are regarded as analgous to S and C planes. The number and extent of seams, the amount of dissolution they indicate, and the efficiency of deformation partitioning imply some enhancement of chemical activity and substantial silica loss from the system. This, in turn, suggests the passage of large amount of silica-undersaturated fluid, and melanges may be zones of high fluid flow. However, the microstructures and the disruptive nature of the fabrics may also reflect the influence of high bulk shear strains and suggest some relationship between the shearing component of deformation and the development of cleavages and foliations." @default.
• W2165200576 created "2016-06-24" @default.
• W2165200576 creator A5003578300 @default.
• W2165200576 date "1987-04-01" @default.
• W2165200576 modified "2023-10-09" @default.
• W2165200576 title "The influence of deformation partitioning on dissolution and solution transfer in low-grade tectonic mélange" @default.
• W2165200576 cites W1970565634 @default.
• W2165200576 cites W1970952468 @default.
• W2165200576 cites W1973666742 @default.
• W2165200576 cites W1975304447 @default.
• W2165200576 cites W1979834892 @default.
• W2165200576 cites W1987435502 @default.
• W2165200576 cites W1989366984 @default.
• W2165200576 cites W1996127304 @default.
• W2165200576 cites W1999098671 @default.
• W2165200576 cites W1999337372 @default.
• W2165200576 cites W2003367767 @default.
• W2165200576 cites W2005093955 @default.
• W2165200576 cites W2006627386 @default.
• W2165200576 cites W2007679470 @default.
• W2165200576 cites W2013069443 @default.
• W2165200576 cites W2015035949 @default.
• W2165200576 cites W2023700907 @default.
• W2165200576 cites W2037488080 @default.
• W2165200576 cites W2037674312 @default.
• W2165200576 cites W2040227616 @default.
• W2165200576 cites W2041883675 @default.
• W2165200576 cites W2046022281 @default.
• W2165200576 cites W2046696482 @default.
• W2165200576 cites W2048503666 @default.
• W2165200576 cites W2052058731 @default.
• W2165200576 cites W2056938420 @default.
• W2165200576 cites W2068532169 @default.
• W2165200576 cites W2073235370 @default.
• W2165200576 cites W2078283387 @default.
• W2165200576 cites W2084133311 @default.
• W2165200576 cites W2085747978 @default.
• W2165200576 cites W2102064893 @default.
• W2165200576 cites W2109281784 @default.
• W2165200576 cites W2111555634 @default.
• W2165200576 cites W2115035416 @default.
• W2165200576 cites W2115460911 @default.
• W2165200576 cites W2115633647 @default.
• W2165200576 cites W2143501565 @default.
• W2165200576 cites W2152058039 @default.
• W2165200576 cites W2162266220 @default.
• W2165200576 cites W2164452015 @default.
• W2165200576 cites W2167888127 @default.
• W2165200576 cites W2207106615 @default.
• W2165200576 cites W2217851118 @default.
• W2165200576 cites W2313457781 @default.
• W2165200576 cites W2318133826 @default.
• W2165200576 cites W2329195711 @default.
• W2165200576 cites W2331783168 @default.
• W2165200576 cites W2334204322 @default.
• W2165200576 cites W2894781993 @default.
• W2165200576 cites W2968600911 @default.
• W2165200576 cites W4229601275 @default.
• W2165200576 doi "https://doi.org/10.1111/j.1525-1314.1987.tb00379.x" @default.
• W2165200576 hasPublicationYear "1987" @default.
• W2165200576 type Work @default.
• W2165200576 sameAs 2165200576 @default.
• W2165200576 citedByCount "33" @default.
• W2165200576 countsByYear W21652005762018 @default.
• W2165200576 crossrefType "journal-article" @default.
• W2165200576 hasAuthorship W2165200576A5003578300 @default.
• W2165200576 hasConcept C127313418 @default.
• W2165200576 hasConcept C13106087 @default.
• W2165200576 hasConcept C133916931 @default.
• W2165200576 hasConcept C147789679 @default.
• W2165200576 hasConcept C151730666 @default.
• W2165200576 hasConcept C152279782 @default.
• W2165200576 hasConcept C165205528 @default.
• W2165200576 hasConcept C17409809 @default.
• W2165200576 hasConcept C175156509 @default.
• W2165200576 hasConcept C185592680 @default.
• W2165200576 hasConcept C187320778 @default.
• W2165200576 hasConcept C199289684 @default.
• W2165200576 hasConcept C2779870107 @default.
• W2165200576 hasConcept C2780191791 @default.
• W2165200576 hasConcept C43369102 @default.
• W2165200576 hasConcept C5900021 @default.
• W2165200576 hasConcept C6494504 @default.
• W2165200576 hasConcept C77928131 @default.
• W2165200576 hasConcept C88380143 @default.
• W2165200576 hasConcept C96035792 @default.
• W2165200576 hasConceptScore W2165200576C127313418 @default.
• W2165200576 hasConceptScore W2165200576C13106087 @default.
• W2165200576 hasConceptScore W2165200576C133916931 @default.
• W2165200576 hasConceptScore W2165200576C147789679 @default.
• W2165200576 hasConceptScore W2165200576C151730666 @default.
• W2165200576 hasConceptScore W2165200576C152279782 @default.
• W2165200576 hasConceptScore W2165200576C165205528 @default.
• W2165200576 hasConceptScore W2165200576C17409809 @default.
• W2165200576 hasConceptScore W2165200576C175156509 @default.
• W2165200576 hasConceptScore W2165200576C185592680 @default.
• W2165200576 hasConceptScore W2165200576C187320778 @default.
• W2165200576 hasConceptScore W2165200576C199289684 @default.

• next