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Description
  • Euhedral pseudoleucite megacrysts (up to 20 cm) occurs in dykes of porphyritic phonolites representing youngest derivatives of the Cenozoic Loučná–Oberwiesenthal Volcanic Centre. Pseudoleucite comprises aggregates of totally prevailing K-feldspar (80-90 %), minor constituens are dioctahedral 1 M muscovite and relict analcime. The pseudoleucites have grown in three stages: (1) crystallisation of initial leucite, (2) transformation of leucite to analcime, and (3) crystalisation of K-feldspar at the expense of leucite and nalacime.
  • Euhedral pseudoleucite megacrysts (up to 20 cm) occurs in dykes of porphyritic phonolites representing youngest derivatives of the Cenozoic Loučná–Oberwiesenthal Volcanic Centre. Pseudoleucite comprises aggregates of totally prevailing K-feldspar (80-90 %), minor constituens are dioctahedral 1 M muscovite and relict analcime. The pseudoleucites have grown in three stages: (1) crystallisation of initial leucite, (2) transformation of leucite to analcime, and (3) crystalisation of K-feldspar at the expense of leucite and nalacime. (en)
  • Idiomorfní pseudoleucitové megakrysty se vyskytují v žilách porfyrických fonolitů, které representují nejmladší deriváty kenozoického Loučná–Oberwiesenthalského vulkanického centra. Pseudoleucit je tvořen agregáty zcela převládajícího K-živce (80-90 %), minoritní komponenty jsou dioktaedrický 1 M muskovit a reliktní analcim. Pseudoleucity vznikaly ve třech stádiích: (1) krystallizace původního leucitu, (2) transformace leucitu na analcim a (3) krystalizace K-živce na na úkor leucitu a analcimu. (cs)
Title
  • On the origin of pseudoleucite from Cenozoic phonolite dykes from Loučná/Böhmisch Wiesenthal, Krušné hory/Erzgebirge Mts., Bohemia
  • Původ pseudoleucitu z kenozoicých fonolitových žil z Loučné/Böhmisch Wiesenthal v Krušných horách/Erzgebirge, Čechy (cs)
  • On the origin of pseudoleucite from Cenozoic phonolite dykes from Loučná/Böhmisch Wiesenthal, Krušné hory/Erzgebirge Mts., Bohemia (en)
skos:prefLabel
  • On the origin of pseudoleucite from Cenozoic phonolite dykes from Loučná/Böhmisch Wiesenthal, Krušné hory/Erzgebirge Mts., Bohemia
  • Původ pseudoleucitu z kenozoicých fonolitových žil z Loučné/Böhmisch Wiesenthal v Krušných horách/Erzgebirge, Čechy (cs)
  • On the origin of pseudoleucite from Cenozoic phonolite dykes from Loučná/Böhmisch Wiesenthal, Krušné hory/Erzgebirge Mts., Bohemia (en)
skos:notation
  • RIV/67985831:_____/04:00000391!RIV/2005/AV0/A09005/N
http://linked.open.../vavai/riv/strany
  • 221;238
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(IAA3048201)
http://linked.open...iv/cisloPeriodika
  • 3
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 577910
http://linked.open...ai/riv/idVysledku
  • RIV/67985831:_____/04:00000391
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • pseudoleucite; phonolite; tinguaite; dyke; mineralogy; petrology; Cenozoic; Krušné hory/Erzgebirge Mts.; Bohemian Massif (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • DE - Spolková republika Německo
http://linked.open...ontrolniKodProRIV
  • [3190EF0EFAC7]
http://linked.open...i/riv/nazevZdroje
  • Neues Jahrbuch für Mineralogie
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 179
http://linked.open...iv/tvurceVysledku
  • Ulrych, Jaromír
  • Langrová, Anna
  • Pivec, Edvín
issn
  • 0028-3649
number of pages
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