Detail publikace

Tachylyte in Cenozoic basaltic lavas from the Czech Republic and Iceland: contrasting compositional trends

ULRYCH, J. KRMÍČEK, L. TESCHNER, C. ŘANDA, Z. SKÁLA, R. JONÁŠOVÁ, Š. FEDIUK, F. ADAMOVIČ, J. POKORNÝ, R.

Originální název

Tachylyte in Cenozoic basaltic lavas from the Czech Republic and Iceland: contrasting compositional trends

Typ

článek v časopise ve Web of Science, Jimp

Jazyk

angličtina

Originální abstrakt

Tachylytes in alkaline rift-related volcanic rocks were recognized in three geological positions: (i) irregular veinlets and fillings of cavities in host alkaline lava flows of the Kozákov volcano, Czech Republic, (ii) (sub)angular xenoliths in alkaline lava of the feeding channel of the Bukovec volcano, Czech Republic, and (iii) paleosurface of a tholeiitic lava flow from Hafrafell volcano, Iceland. The tachylyte from Kozákov displays phonotephrite to tephriphonolite whole-rock composition while that from Bukovec exhibits trachyandesite to tephriphonolite geochemistry. Host rocks at the two sites are of basanite composition. Both glass and host rock from Hafrafell are of tholeiitic basalt composition. The tachylyte from Kozákov, compared with the host rock, revealed a substantial enrichment in major elements such as SiO2, Al2O3, Na2O, K2O and H2O, associated with a depletion in MgO and Fetot. The contents of incompatible elements such as Rb, Sr, Ba, Nb, Zr, REE, Th and U in the tachylyte are higher than those in the host rocks. The tachylyte from Bukovec displays partly similar trends in major element contents but contrasting trends in the incompatible element contents. The similarity in chemical composition of the Hafrafell tachylyte paleosurface layer and parental tholeiitic basalt is characteristic for lava extrusions. The host/parent rocks and tachylytes have similar initial Sr–Nd characteristics testifying for their co-magmatic sources. The initial epsilon(Nd) values of host/parent rocks and tachylytes from the Bohemian Massif (3.4 to 3.9) and those from Iceland (6.3) are interpreted as primary magma values. Only the tachylyte from Bukovec shows a different epsilon(Nd) value of -2.1, corresponding to a xenolith of primarily sedimentary/metamorphic origin.

Klíčová slova

basaltic glass; major genetic types; rift-related volcanites; mineral composition; chemical composition; Sr-Nd isotopes

Autoři

ULRYCH, J.; KRMÍČEK, L.; TESCHNER, C.; ŘANDA, Z.; SKÁLA, R.; JONÁŠOVÁ, Š.; FEDIUK, F.; ADAMOVIČ, J.; POKORNÝ, R.

Vydáno

30. 9. 2017

Nakladatel

Springer Verlag

Místo

Vídeň

ISSN

0930-0708

Periodikum

MINERALOGY AND PETROLOGY

Ročník

111

Číslo

5

Stát

Rakouská republika

Strany od

761

Strany do

775

Strany počet

15

BibTex

@article{BUT139930,
  author="ULRYCH, J. and KRMÍČEK, L. and TESCHNER, C. and ŘANDA, Z. and SKÁLA, R. and JONÁŠOVÁ, Š. and FEDIUK, F. and ADAMOVIČ, J. and POKORNÝ, R.",
  title="Tachylyte in Cenozoic basaltic lavas from the Czech Republic and Iceland: contrasting compositional trends",
  journal="MINERALOGY AND PETROLOGY",
  year="2017",
  volume="111",
  number="5",
  pages="761--775",
  doi="10.1007/s00710-016-0483-x",
  issn="0930-0708"
}