FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2135785473> ?p ?o ?g. }

• W2135785473 endingPage "1659" @default.
• W2135785473 startingPage "1645" @default.
• W2135785473 abstract "The 1.57 Ga Eurajoki stock in southwestern Finland is composed of biotite–hornblende–fayalite granite, biotite granites and late-stage topaz-bearing granite, as well as related topaz-bearing rhyolite (ongonite) dykes. Miarolitic cavities indicate the presence of a separate fluid phase during late stages of crystallization of topaz-bearing granite, and greisen-type Sn–Be–W–Zn mineralization is closely associated with it. Subsolidus reactions have modified the petrography and geochemistry of the topaz-bearing granite. The presence of magmatic topaz is indicated by petrographic features and crystallized melt inclusions entrapped in topaz. The magmatic origin of accessory cassiterite in the topaz-bearing granite (average 80 ppm Sn) is indicated by mode of occurrence and chemical composition of cassiterite: the Nb2O5 + Ta2O5 content of cassiterite is 4.8–8.7 wt % in granite, 2.3–3% in pegmatite and 0.0–0.6% in greisen. Some of the rhyolite dykes contain topaz as phenocrysts and as small prismatic crystals in the groundmass showing locally fluidal texture. These features indicate that the late-stage magma was highly enriched in F and Sn. Strong exsolution of alkali feldspar has produced intergranular albite rims and grain rows. De-anorthitization of primary plagioclase has produced turbid albite with inclusions of topaz, fluorite and quartz. Metasomatic albitization of K-feldspar and K-feldspathization of plagioclase have only locally been important. In greisenized granite, metasomatic addition of topaz and quartz is common. The topaz-bearing granite had originally anomalous geochemistry and mineralogy, and its anomalous character was further increased during postmagmatic fluid–rock interaction. The petrographic and geochemical peculiarities of the topaz–bearing granite of Eurajoki are characteristic of many other late-stage intrusive phases of rapakivi complexes and for many tin granites of different ages. In interpreting the origin of such highly evolved granites, the role of Na-metasomatic albitization has often been overemphasized at the expense of exsolution and recrystallization." @default.
• W2135785473 created "2016-06-24" @default.
• W2135785473 creator A5003669807 @default.
• W2135785473 date "1997-12-01" @default.
• W2135785473 modified "2023-10-03" @default.
• W2135785473 title "Magmatic and Postmagmatic Processes in Tin-mineralized Granites: Topaz-bearing Leucogranite in the Eurajoki Rapakivi Granite Stock, Finland" @default.
• W2135785473 cites W1514627894 @default.
• W2135785473 cites W1623750096 @default.
• W2135785473 cites W1966555528 @default.
• W2135785473 cites W1966766530 @default.
• W2135785473 cites W1971772202 @default.
• W2135785473 cites W1975534655 @default.
• W2135785473 cites W1978299523 @default.
• W2135785473 cites W1979418505 @default.
• W2135785473 cites W1982386179 @default.
• W2135785473 cites W1989064331 @default.
• W2135785473 cites W2013663553 @default.
• W2135785473 cites W2019372598 @default.
• W2135785473 cites W2023926717 @default.
• W2135785473 cites W2052681045 @default.
• W2135785473 cites W2073185915 @default.
• W2135785473 cites W2078180163 @default.
• W2135785473 cites W2087025316 @default.
• W2135785473 cites W2103578787 @default.
• W2135785473 cites W2119167301 @default.
• W2135785473 cites W2126539747 @default.
• W2135785473 cites W2146521976 @default.
• W2135785473 cites W2167528749 @default.
• W2135785473 cites W2405272450 @default.
• W2135785473 cites W2415081471 @default.
• W2135785473 cites W2604771354 @default.
• W2135785473 cites W2607204968 @default.
• W2135785473 cites W268086059 @default.
• W2135785473 cites W2746725828 @default.
• W2135785473 cites W4293580270 @default.
• W2135785473 doi "https://doi.org/10.1093/petroj/38.12.1645" @default.
• W2135785473 hasPublicationYear "1997" @default.
• W2135785473 type Work @default.
• W2135785473 sameAs 2135785473 @default.
• W2135785473 citedByCount "117" @default.
• W2135785473 countsByYear W21357854732012 @default.
• W2135785473 countsByYear W21357854732013 @default.
• W2135785473 countsByYear W21357854732014 @default.
• W2135785473 countsByYear W21357854732015 @default.
• W2135785473 countsByYear W21357854732016 @default.
• W2135785473 countsByYear W21357854732017 @default.
• W2135785473 countsByYear W21357854732018 @default.
• W2135785473 countsByYear W21357854732019 @default.
• W2135785473 countsByYear W21357854732020 @default.
• W2135785473 countsByYear W21357854732021 @default.
• W2135785473 countsByYear W21357854732022 @default.
• W2135785473 countsByYear W21357854732023 @default.
• W2135785473 crossrefType "journal-article" @default.
• W2135785473 hasAuthorship W2135785473A5003669807 @default.
• W2135785473 hasBestOaLocation W21357854731 @default.
• W2135785473 hasConcept C120806208 @default.
• W2135785473 hasConcept C127313418 @default.
• W2135785473 hasConcept C151730666 @default.
• W2135785473 hasConcept C171701179 @default.
• W2135785473 hasConcept C17409809 @default.
• W2135785473 hasConcept C178790620 @default.
• W2135785473 hasConcept C182402614 @default.
• W2135785473 hasConcept C185592680 @default.
• W2135785473 hasConcept C192241223 @default.
• W2135785473 hasConcept C25822816 @default.
• W2135785473 hasConcept C26687426 @default.
• W2135785473 hasConcept C2775859737 @default.
• W2135785473 hasConcept C2776152364 @default.
• W2135785473 hasConcept C2777229588 @default.
• W2135785473 hasConcept C2777825866 @default.
• W2135785473 hasConcept C2779181077 @default.
• W2135785473 hasConcept C2779526359 @default.
• W2135785473 hasConcept C2779532088 @default.
• W2135785473 hasConcept C2779642852 @default.
• W2135785473 hasConcept C2779670319 @default.
• W2135785473 hasConcept C2779870107 @default.
• W2135785473 hasConcept C37282123 @default.
• W2135785473 hasConcept C525849907 @default.
• W2135785473 hasConcept C542268612 @default.
• W2135785473 hasConceptScore W2135785473C120806208 @default.
• W2135785473 hasConceptScore W2135785473C127313418 @default.
• W2135785473 hasConceptScore W2135785473C151730666 @default.
• W2135785473 hasConceptScore W2135785473C171701179 @default.
• W2135785473 hasConceptScore W2135785473C17409809 @default.
• W2135785473 hasConceptScore W2135785473C178790620 @default.
• W2135785473 hasConceptScore W2135785473C182402614 @default.
• W2135785473 hasConceptScore W2135785473C185592680 @default.
• W2135785473 hasConceptScore W2135785473C192241223 @default.
• W2135785473 hasConceptScore W2135785473C25822816 @default.
• W2135785473 hasConceptScore W2135785473C26687426 @default.
• W2135785473 hasConceptScore W2135785473C2775859737 @default.
• W2135785473 hasConceptScore W2135785473C2776152364 @default.
• W2135785473 hasConceptScore W2135785473C2777229588 @default.
• W2135785473 hasConceptScore W2135785473C2777825866 @default.
• W2135785473 hasConceptScore W2135785473C2779181077 @default.
• W2135785473 hasConceptScore W2135785473C2779526359 @default.
• W2135785473 hasConceptScore W2135785473C2779532088 @default.
• W2135785473 hasConceptScore W2135785473C2779642852 @default.

• next