Matches in SemOpenAlex for { <https://semopenalex.org/work/W2088143372> ?p ?o ?g. }
- W2088143372 endingPage "722" @default.
- W2088143372 startingPage "703" @default.
- W2088143372 abstract "Abstract The evolution of the trace-element patterns of quartz during crystallization of pegmatite melt was investigated using laser ablation inductively coupled plasma mass spectrometry. The contents of Al, B, Ba, Be, Cr, Fe, Ge, Li, Mn, P, Rb, Sn, Sr and Ti were analysed in quartz from the border, intermediate and core zones of four granitic pegmatites differing in degree of fractionation and origin. The material investigated originates from the pegmatite district of the Strážek Unit, Moldanubian Zone, Bohemian Massif, Czech Republic and includes: lepidolite LCT (Li-Cs-Ta) pegmatite from Rožná; berylcolumbite LCT pegmatite from Věžná; anatectic pegmatite from Znětínek; and intragranitic NYF (Nb-Y-F) pegmatite Vladislav from the Třebíč Pluton. The abundances of the elements analysed varied over wide intervals: <1 to 32 ppm Li, 0.5 to 6 ppm B, <1 to 10 ppm Ge, 1 to 10 ppm P, 10 to 450 ppm Al, 1 to 45 ppm Ti and <1 to 40 ppm Fe (average sample contents). Concentrations of Be, Rb, Sr, Sn, Ba, Cr and Mn are usually <1 ppm. Quartz from LCT pegmatites exhibits a distinct evolutionary trend with a decrease in Ti and an increase in Al, Li and Ge from the pegmatite border to the core. In comparison with the most fractionated rare-metal granites, pegmatitic quartz is relatively depleted in Al and Li, but strongly enriched in Ge. Quartz from simple anatectic and NYF pegmatites is poor in all trace elements with their evolution marked by a decrease in Ti and a small increase in Ge. There is little Al or Li and neither shows any systematic change with pegmatite evolution. Using the Ti-in-quartz thermobarometer, the outer zones of the Znětínek and Vladislav pegmatites crystallized at ∼670°C, whereas the border zone in the Rožná pegmatite yields a temperature near 610°C." @default.
- W2088143372 created "2016-06-24" @default.
- W2088143372 creator A5011653485 @default.
- W2088143372 creator A5030470807 @default.
- W2088143372 creator A5037933533 @default.
- W2088143372 creator A5070421855 @default.
- W2088143372 creator A5082486038 @default.
- W2088143372 date "2014-06-01" @default.
- W2088143372 modified "2023-10-06" @default.
- W2088143372 title "Trace element composition of quartz from different types of pegmatites: A case study from the Moldanubian Zone of the Bohemian Massif (Czech Republic)" @default.
- W2088143372 cites W1493867994 @default.
- W2088143372 cites W1965038649 @default.
- W2088143372 cites W1965107179 @default.
- W2088143372 cites W1969135086 @default.
- W2088143372 cites W1970288815 @default.
- W2088143372 cites W1982925963 @default.
- W2088143372 cites W1987348854 @default.
- W2088143372 cites W1993269052 @default.
- W2088143372 cites W1993386061 @default.
- W2088143372 cites W1994405980 @default.
- W2088143372 cites W2011488152 @default.
- W2088143372 cites W2013066483 @default.
- W2088143372 cites W2013566102 @default.
- W2088143372 cites W2027822014 @default.
- W2088143372 cites W2029351912 @default.
- W2088143372 cites W2039532320 @default.
- W2088143372 cites W2052443456 @default.
- W2088143372 cites W2068226577 @default.
- W2088143372 cites W2070951810 @default.
- W2088143372 cites W2074388765 @default.
- W2088143372 cites W2079846923 @default.
- W2088143372 cites W2080271111 @default.
- W2088143372 cites W2080539747 @default.
- W2088143372 cites W2083548465 @default.
- W2088143372 cites W2084317102 @default.
- W2088143372 cites W2085064498 @default.
- W2088143372 cites W2086984328 @default.
- W2088143372 cites W2089038685 @default.
- W2088143372 cites W2089461947 @default.
- W2088143372 cites W2101458885 @default.
- W2088143372 cites W2103773436 @default.
- W2088143372 cites W2113248441 @default.
- W2088143372 cites W2136488494 @default.
- W2088143372 cites W2138769772 @default.
- W2088143372 cites W2149433394 @default.
- W2088143372 cites W2151553735 @default.
- W2088143372 cites W2152547485 @default.
- W2088143372 cites W2170205984 @default.
- W2088143372 cites W2226614280 @default.
- W2088143372 cites W2316524128 @default.
- W2088143372 cites W2325553588 @default.
- W2088143372 cites W2328214548 @default.
- W2088143372 cites W2329950245 @default.
- W2088143372 cites W2331011456 @default.
- W2088143372 cites W2336452864 @default.
- W2088143372 cites W256261911 @default.
- W2088143372 cites W2606595536 @default.
- W2088143372 doi "https://doi.org/10.1180/minmag.2014.078.3.17" @default.
- W2088143372 hasPublicationYear "2014" @default.
- W2088143372 type Work @default.
- W2088143372 sameAs 2088143372 @default.
- W2088143372 citedByCount "32" @default.
- W2088143372 countsByYear W20881433722015 @default.
- W2088143372 countsByYear W20881433722016 @default.
- W2088143372 countsByYear W20881433722017 @default.
- W2088143372 countsByYear W20881433722018 @default.
- W2088143372 countsByYear W20881433722019 @default.
- W2088143372 countsByYear W20881433722020 @default.
- W2088143372 countsByYear W20881433722021 @default.
- W2088143372 countsByYear W20881433722022 @default.
- W2088143372 countsByYear W20881433722023 @default.
- W2088143372 crossrefType "journal-article" @default.
- W2088143372 hasAuthorship W2088143372A5011653485 @default.
- W2088143372 hasAuthorship W2088143372A5030470807 @default.
- W2088143372 hasAuthorship W2088143372A5037933533 @default.
- W2088143372 hasAuthorship W2088143372A5070421855 @default.
- W2088143372 hasAuthorship W2088143372A5082486038 @default.
- W2088143372 hasConcept C127313418 @default.
- W2088143372 hasConcept C134132462 @default.
- W2088143372 hasConcept C151730666 @default.
- W2088143372 hasConcept C160776313 @default.
- W2088143372 hasConcept C17409809 @default.
- W2088143372 hasConcept C191897082 @default.
- W2088143372 hasConcept C192562407 @default.
- W2088143372 hasConcept C195845463 @default.
- W2088143372 hasConcept C199289684 @default.
- W2088143372 hasConcept C2779870107 @default.
- W2088143372 hasConcept C2780861898 @default.
- W2088143372 hasConceptScore W2088143372C127313418 @default.
- W2088143372 hasConceptScore W2088143372C134132462 @default.
- W2088143372 hasConceptScore W2088143372C151730666 @default.
- W2088143372 hasConceptScore W2088143372C160776313 @default.
- W2088143372 hasConceptScore W2088143372C17409809 @default.
- W2088143372 hasConceptScore W2088143372C191897082 @default.
- W2088143372 hasConceptScore W2088143372C192562407 @default.
- W2088143372 hasConceptScore W2088143372C195845463 @default.
- W2088143372 hasConceptScore W2088143372C199289684 @default.
- W2088143372 hasConceptScore W2088143372C2779870107 @default.