| HALODA, Jakub, Vladislav RAPPRICH, Frantisek V HOLUB, Patricie HALODOVA a Tomáš VACULOVIČ. Crystallization history of Oligocene ijolitic rocks from the Doupovske hory Volcanic Complex (Czech Republic). Arabian Journal of Geosciences. HEIDELBERG, GERMANY: SPRINGER HEIDELBERG, 2010, roč. 55, č. 3, s. 279-297. ISSN 1866-7511. Dostupné z: https://dx.doi.org/10.3190/jgeosci.076. |
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@article{1664021,
author = {Haloda, Jakub and Rapprich, Vladislav and Holub, Frantisek V and Halodova, Patricie and Vaculovič, Tomáš},
article_location = {HEIDELBERG, GERMANY},
article_number = {3},
doi = {http://dx.doi.org/10.3190/jgeosci.076},
keywords = {Nephelinolite; melteigite; ijolite; crystallization modelling; fractional crystallization; Doupovske hory Mts.},
language = {eng},
issn = {1866-7511},
journal = {Arabian Journal of Geosciences},
title = {Crystallization history of Oligocene ijolitic rocks from the Doupovske hory Volcanic Complex (Czech Republic)},
url = {http://dx.doi.org/10.3190/jgeosci.076},
volume = {55},
year = {2010}
}
TY - JOUR
ID - 1664021
AU - Haloda, Jakub - Rapprich, Vladislav - Holub, Frantisek V - Halodova, Patricie - Vaculovič, Tomáš
PY - 2010
TI - Crystallization history of Oligocene ijolitic rocks from the Doupovske hory Volcanic Complex (Czech Republic)
JF - Arabian Journal of Geosciences
VL - 55
IS - 3
SP - 279-297
EP - 279-297
PB - SPRINGER HEIDELBERG
SN - 18667511
KW - Nephelinolite
KW - melteigite
KW - ijolite
KW - crystallization modelling
KW - fractional crystallization
KW - Doupovske hory Mts.
UR - http://dx.doi.org/10.3190/jgeosci.076
L2 - http://dx.doi.org/10.3190/jgeosci.076
N2 - Ijolitic rocks of the Flurbuhl Composite Intrusion rank to the most primitive intrusive rocks found within the Doupovske hory Volcanic Complex. Studies of mineral chemistry together with crystallization modelling of melteigite and ijolite brought new information about the evolution of ijolitic magmas and their ascent. Crystallization modelling affirms the absence of accumulated minerals and confirms that the recalculated major-element bulk-rock analyses reflect the compositions of their original parental magmas accurately. Melteigite developed by early equilibrium crystallization under pressure of approximately 4 kbar (estimated minimum cooling rate is similar to 0.02 degrees C/hr) and subsequent fractional crystallization under much lower pressure (similar to 0.2 kbar). Ijolite originated by fractional crystallization of a slightly more evolved magma batch under lower pressures probably at the final emplacement level. The results of crystallization modelling and estimates of REE contents in parental melts suggest a close genetic relationship between both rock suites. The olivine-bearing melteigite was postulated as a possible parental magma composition for derivation of the olivine-free ijolite.
ER -
HALODA, Jakub, Vladislav RAPPRICH, Frantisek V HOLUB, Patricie HALODOVA a Tomáš VACULOVIČ. Crystallization history of Oligocene ijolitic rocks from the Doupovske hory Volcanic Complex (Czech Republic). \textit{Arabian Journal of Geosciences}. HEIDELBERG, GERMANY: SPRINGER HEIDELBERG, 2010, roč.~55, č.~3, s.~279-297. ISSN~1866-7511. Dostupné z: https://dx.doi.org/10.3190/jgeosci.076.
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