FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2023056733> ?p ?o ?g. }

• W2023056733 abstract "Abstract In the Molanite Valley west of Mt. Isa, tremolite-bearing metasomatic pods, showing sharp contacts with enclosing rocks, occur over a strike length of 7.4 km in the biotite-zone Bortala Formation. In relatively low-strain rocks of the western part of the valley, plagioclase—tremolite pods have replaced psammite or mica schist surrounding the terminations of buck quartz veins, whereas in intensively sheared rocks to the east, pods of medium to coarse-grained massive tremolite (commonly containing greater than 95% tremolite) have replaced marble, quartzite and psammite. Talc-chlorite schists, formed by dissolution of carbonates during shearing of marble, are associated with some of the massive tremolite pods. The direct relationship between structural domains and metasomatism suggests that migration of externally-derived fluids was controlled by fractures and the shear zone. The fluids, having migrated along fractures, interacted with wall rocks to produce plagioclase-tremolite pods. In the shear zone, buck quartz veins, some tremolite-bearing, show no obvious geometric relationship to massive tremolite pods. It is postulated that the metasomatic fluids fluxed through shear domains and penetrated progressive shortening domains to replace the host rocks and form the massive tremolite pods. Both styles of metasomatic rocks developed from late S 2 to early S 3 during a progressive E-W shortening event, which corresponds to the regional metamorphism. The metasomatic rocks represent only a small part of widespread metasomatism across the Mt. Isa Inlier." @default.
• W2023056733 created "2016-06-24" @default.
• W2023056733 creator A5026332381 @default.
• W2023056733 creator A5081344075 @default.
• W2023056733 date "1995-01-01" @default.
• W2023056733 modified "2023-09-27" @default.
• W2023056733 title "Structural controls on syntectonic metasomatic tremolite and tremolite-plagioclase pods in the Molanite Valley, Mt. Isa, Australia" @default.
• W2023056733 cites W109763388 @default.
• W2023056733 cites W1493074749 @default.
• W2023056733 cites W1928320224 @default.
• W2023056733 cites W1968812062 @default.
• W2023056733 cites W1971497103 @default.
• W2023056733 cites W1972761424 @default.
• W2023056733 cites W1972909865 @default.
• W2023056733 cites W1994466040 @default.
• W2023056733 cites W2003367767 @default.
• W2023056733 cites W2006667472 @default.
• W2023056733 cites W2016513825 @default.
• W2023056733 cites W2023327969 @default.
• W2023056733 cites W2023553073 @default.
• W2023056733 cites W2030155465 @default.
• W2023056733 cites W2045447627 @default.
• W2023056733 cites W2065988409 @default.
• W2023056733 cites W2070663124 @default.
• W2023056733 cites W2072830841 @default.
• W2023056733 cites W2086540298 @default.
• W2023056733 cites W2087881480 @default.
• W2023056733 cites W2088168225 @default.
• W2023056733 cites W2110481460 @default.
• W2023056733 cites W2140408185 @default.
• W2023056733 cites W2144371413 @default.
• W2023056733 cites W2156930601 @default.
• W2023056733 cites W2161009656 @default.
• W2023056733 cites W2319095826 @default.
• W2023056733 cites W2586616728 @default.
• W2023056733 cites W3035643309 @default.
• W2023056733 cites W357897758 @default.
• W2023056733 doi "https://doi.org/10.1016/0191-8141(94)e0021-p" @default.
• W2023056733 hasPublicationYear "1995" @default.
• W2023056733 type Work @default.
• W2023056733 sameAs 2023056733 @default.
• W2023056733 citedByCount "14" @default.
• W2023056733 countsByYear W20230567332012 @default.
• W2023056733 countsByYear W20230567332013 @default.
• W2023056733 countsByYear W20230567332014 @default.
• W2023056733 crossrefType "journal-article" @default.
• W2023056733 hasAuthorship W2023056733A5026332381 @default.
• W2023056733 hasAuthorship W2023056733A5081344075 @default.
• W2023056733 hasConcept C101139013 @default.
• W2023056733 hasConcept C112764850 @default.
• W2023056733 hasConcept C127313418 @default.
• W2023056733 hasConcept C151730666 @default.
• W2023056733 hasConcept C167919410 @default.
• W2023056733 hasConcept C17409809 @default.
• W2023056733 hasConcept C191897082 @default.
• W2023056733 hasConcept C192562407 @default.
• W2023056733 hasConcept C26687426 @default.
• W2023056733 hasConcept C2778302498 @default.
• W2023056733 hasConcept C2779181077 @default.
• W2023056733 hasConcept C2779870107 @default.
• W2023056733 hasConcept C510490043 @default.
• W2023056733 hasConcept C67236022 @default.
• W2023056733 hasConceptScore W2023056733C101139013 @default.
• W2023056733 hasConceptScore W2023056733C112764850 @default.
• W2023056733 hasConceptScore W2023056733C127313418 @default.
• W2023056733 hasConceptScore W2023056733C151730666 @default.
• W2023056733 hasConceptScore W2023056733C167919410 @default.
• W2023056733 hasConceptScore W2023056733C17409809 @default.
• W2023056733 hasConceptScore W2023056733C191897082 @default.
• W2023056733 hasConceptScore W2023056733C192562407 @default.
• W2023056733 hasConceptScore W2023056733C26687426 @default.
• W2023056733 hasConceptScore W2023056733C2778302498 @default.
• W2023056733 hasConceptScore W2023056733C2779181077 @default.
• W2023056733 hasConceptScore W2023056733C2779870107 @default.
• W2023056733 hasConceptScore W2023056733C510490043 @default.
• W2023056733 hasConceptScore W2023056733C67236022 @default.
• W2023056733 hasLocation W20230567331 @default.
• W2023056733 hasOpenAccess W2023056733 @default.
• W2023056733 hasPrimaryLocation W20230567331 @default.
• W2023056733 hasRelatedWork W1838986098 @default.
• W2023056733 hasRelatedWork W1971497103 @default.
• W2023056733 hasRelatedWork W1975482900 @default.
• W2023056733 hasRelatedWork W1982625888 @default.
• W2023056733 hasRelatedWork W1996385203 @default.
• W2023056733 hasRelatedWork W1998285411 @default.
• W2023056733 hasRelatedWork W2003584880 @default.
• W2023056733 hasRelatedWork W2006667472 @default.
• W2023056733 hasRelatedWork W2009466418 @default.
• W2023056733 hasRelatedWork W2011308336 @default.
• W2023056733 hasRelatedWork W2019392649 @default.
• W2023056733 hasRelatedWork W2050103121 @default.
• W2023056733 hasRelatedWork W2061312893 @default.
• W2023056733 hasRelatedWork W2071025161 @default.
• W2023056733 hasRelatedWork W2075525876 @default.
• W2023056733 hasRelatedWork W2080564426 @default.
• W2023056733 hasRelatedWork W2081202204 @default.
• W2023056733 hasRelatedWork W2087881480 @default.
• W2023056733 hasRelatedWork W2132138546 @default.
• W2023056733 hasRelatedWork W2327399076 @default.
• W2023056733 isParatext "false" @default.

• next