Detailed Information on Publication Record
2007
Compositional evolution and substitutions in disseminated and nodular tourmaline from leucocratic granites: Examples from the Bohemian Massif, Czech Republic
BURIÁNEK, David and Milan NOVÁKBasic information
Original name
Compositional evolution and substitutions in disseminated and nodular tourmaline from leucocratic granites: Examples from the Bohemian Massif, Czech Republic
Name in Czech
Chemický vývoj a substituce v rozptýlených a nodulárních turmalínech z leukokrátních granitů: Příklad z Českého masivu, Český masiv
Authors
BURIÁNEK, David (203 Czech Republic) and Milan NOVÁK (203 Czech Republic, guarantor)
Edition
Lithos, 2007, 0024-4937
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Norway
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 2.937
RIV identification code
RIV/00216224:14310/07:00022904
Organization unit
Faculty of Science
UT WoS
000245782700012
Keywords in English
tourmaline granite
Tags
Změněno: 25/6/2008 07:23, prof. RNDr. Milan Novák, CSc.
V originále
Two distinct textural types of tourmaline were distinguished in leucocratic granites of the Bohemian Massif (Moldanubicum, Saxothuringicum): (i) commonly euhedral disseminated tourmaline (DT) crystallized in relatively early stage of the granite consolidation, and (ii) typically interstitial nodular tourmaline (NT) formed during the stage transitional from late solidus to early subsolidus crystallization. Very similar chemical composition and similar fractionation trends in both DT and NT tourmaline types indicate crystallization in a quasi-closed system from early solidus to early subsolidus stage of granite consolidation. The substitutions in tourmaline from NT granites in the Moldanubicum are more similar to the substitutions in tourmaline from Li-poor granitic pegmatites in the same region relative to tourmaline from DT granites. Plotting of EMP analyses of tourmaline in diverse diagrams strongly suggests using combination of ternary diagrams Al Fe Mg and Na Ca Xsite vacancy and simple plots involving single cations (elements) such as Na/Al, F/Na, Fe/Mg rather then more complicated diagrams (e.g., R1+R2/R3) to characterize chemical composition and to derive substitution mechanisms in Ca-poor tourmaline from granitic rocks. The complex diagrams e.g., R1+R2 versus R3 do not enable to investigate compositional evolution in the Xsite and Wsite properly and oversimplifies the real substitutions. We recommend using specific diagrams for specific tourmaline compositions (e.g., Carich, Lirich).
In Czech
Byly studovány dva texturně odlišné typy tourmalinu z granitu, jejich chemické slžení a subtituční mechanismy.
Links
MSM0021622412, plan (intention) |
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