Matches in SemOpenAlex for { <https://semopenalex.org/work/W2048148910> ?p ?o ?g. }
- W2048148910 endingPage "336" @default.
- W2048148910 startingPage "327" @default.
- W2048148910 abstract "Various petrologists have suggested that K-feldspar megacrysts grow in granites that are extensively crystallized, even at subsolidus conditions. However, experimental evidence indicates that, though K-feldspar nucleates relatively late in the crystallization history, abundant liquid is available for development of large crystals. A great deal of evidence, involving many different factors, favours a magmatic/phenocrystic origin for K-feldspar megacrysts in granites, namely simple twinning, oscillatory zoning, euhedral plagioclase inclusions, and concentric, crystallographically controlled arrangements of inclusions. In addition, abundant evidence has been presented of (1) mechanical accumulation of K-feldspar megacrysts in granites, (2) alignment of megacrysts and megacryst concentrations in magmatic flow foliations, (3) involvement of megacrysts in zones of magma mixing in granite plutons, and (4) occurrence of megacrysts in some volcanic rocks, implying that the megacrysts were suspended in enough liquid to be moved without fracturing or plastic deformation. Detailed trace element and isotopic data also indicate that megacrysts can move between coexisting felsic and more mafic magmas. Irregular overgrowths on megacrysts are consistent with continued magmatic growth after euhedral megacrystic growth ceased, the overgrowths being impeded by simultaneously crystallizing quartz and feldspar grains." @default.
- W2048148910 created "2016-06-24" @default.
- W2048148910 creator A5003098191 @default.
- W2048148910 creator A5025912806 @default.
- W2048148910 date "2008-08-01" @default.
- W2048148910 modified "2023-10-17" @default.
- W2048148910 title "How late are K-feldspar megacrysts in granites?" @default.
- W2048148910 cites W1964309899 @default.
- W2048148910 cites W1971762124 @default.
- W2048148910 cites W1976028235 @default.
- W2048148910 cites W1980453236 @default.
- W2048148910 cites W1986701070 @default.
- W2048148910 cites W1988057378 @default.
- W2048148910 cites W1991159537 @default.
- W2048148910 cites W1992429612 @default.
- W2048148910 cites W1995382732 @default.
- W2048148910 cites W1997710040 @default.
- W2048148910 cites W1998505479 @default.
- W2048148910 cites W1999256662 @default.
- W2048148910 cites W2004482896 @default.
- W2048148910 cites W2006834372 @default.
- W2048148910 cites W2009822379 @default.
- W2048148910 cites W2012396908 @default.
- W2048148910 cites W2013489290 @default.
- W2048148910 cites W2022732789 @default.
- W2048148910 cites W2026476332 @default.
- W2048148910 cites W2033999508 @default.
- W2048148910 cites W2059835450 @default.
- W2048148910 cites W2063207326 @default.
- W2048148910 cites W2065855118 @default.
- W2048148910 cites W2067799016 @default.
- W2048148910 cites W2069425141 @default.
- W2048148910 cites W2071539087 @default.
- W2048148910 cites W2071706655 @default.
- W2048148910 cites W2073137830 @default.
- W2048148910 cites W2074745063 @default.
- W2048148910 cites W2078013236 @default.
- W2048148910 cites W2087462781 @default.
- W2048148910 cites W2091915995 @default.
- W2048148910 cites W2093488387 @default.
- W2048148910 cites W2093951248 @default.
- W2048148910 cites W2095413393 @default.
- W2048148910 cites W2096680403 @default.
- W2048148910 cites W2098888852 @default.
- W2048148910 cites W2104091804 @default.
- W2048148910 cites W2106079840 @default.
- W2048148910 cites W2107634535 @default.
- W2048148910 cites W2110218619 @default.
- W2048148910 cites W2112313421 @default.
- W2048148910 cites W2112606960 @default.
- W2048148910 cites W2116418789 @default.
- W2048148910 cites W2118493083 @default.
- W2048148910 cites W2133587292 @default.
- W2048148910 cites W2147811982 @default.
- W2048148910 cites W2149913832 @default.
- W2048148910 cites W2152669337 @default.
- W2048148910 cites W2154208726 @default.
- W2048148910 cites W2157508130 @default.
- W2048148910 cites W2164255634 @default.
- W2048148910 cites W2171178261 @default.
- W2048148910 cites W2171966532 @default.
- W2048148910 cites W2256258609 @default.
- W2048148910 cites W2322361841 @default.
- W2048148910 cites W2332142234 @default.
- W2048148910 cites W2340241118 @default.
- W2048148910 cites W2344224945 @default.
- W2048148910 cites W2570630355 @default.
- W2048148910 cites W2747263336 @default.
- W2048148910 cites W4251523230 @default.
- W2048148910 doi "https://doi.org/10.1016/j.lithos.2008.01.001" @default.
- W2048148910 hasPublicationYear "2008" @default.
- W2048148910 type Work @default.
- W2048148910 sameAs 2048148910 @default.
- W2048148910 citedByCount "83" @default.
- W2048148910 countsByYear W20481489102012 @default.
- W2048148910 countsByYear W20481489102013 @default.
- W2048148910 countsByYear W20481489102014 @default.
- W2048148910 countsByYear W20481489102015 @default.
- W2048148910 countsByYear W20481489102017 @default.
- W2048148910 countsByYear W20481489102018 @default.
- W2048148910 countsByYear W20481489102019 @default.
- W2048148910 countsByYear W20481489102020 @default.
- W2048148910 countsByYear W20481489102021 @default.
- W2048148910 countsByYear W20481489102022 @default.
- W2048148910 countsByYear W20481489102023 @default.
- W2048148910 crossrefType "journal-article" @default.
- W2048148910 hasAuthorship W2048148910A5003098191 @default.
- W2048148910 hasAuthorship W2048148910A5025912806 @default.
- W2048148910 hasConcept C11872896 @default.
- W2048148910 hasConcept C120806208 @default.
- W2048148910 hasConcept C127313418 @default.
- W2048148910 hasConcept C151730666 @default.
- W2048148910 hasConcept C167236342 @default.
- W2048148910 hasConcept C167284885 @default.
- W2048148910 hasConcept C17409809 @default.
- W2048148910 hasConcept C183222429 @default.
- W2048148910 hasConcept C193429443 @default.
- W2048148910 hasConcept C195845463 @default.