Detrital zircon populations in quartzites of the Krkonose-Jizera Massif: implications for pre-collisional history of the Saxothuringian Domain in the Bohemian Massif
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F12%3A10126439" target="_blank" >RIV/00216208:11310/12:10126439 - isvavai.cz</a>
Alternative codes found
RIV/00025798:_____/12:00000020
Result on the web
<a href="http://dx.doi.org/10.1017/S0016756811000744" target="_blank" >http://dx.doi.org/10.1017/S0016756811000744</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1017/S0016756811000744" target="_blank" >10.1017/S0016756811000744</a>
Alternative languages
Result language
angličtina
Original language name
Detrital zircon populations in quartzites of the Krkonose-Jizera Massif: implications for pre-collisional history of the Saxothuringian Domain in the Bohemian Massif
Original language description
Age spectra of detrital zircons from metamorphosed quartzites of the Krkonose-Jizera Massif in the northeastern part of the Saxothuringian Domain were obtained by U-Pb laser ablation inductively coupled plasma mass spectrometry dating. The zircon ages cluster in the intervals of 450-530 Ma and 550-670 Ma, and show individual data between 1.6 and 3.1 Ga. Zircons in the analysed samples are predominantly of Cambrian-Ordovician and Neoproterozoic age, and the marked peak at c. 525-500 Ma suggests a late Cambrian maximum age for the sedimentary protolith. Detritus of the quartzites probably originated from the erosion of Cambrian-Ordovician granitoids and their Neoproterozoic (meta) sedimentary or magmatic country rocks. The lack of Neoproterozoic (meta) sedimentary rocks in the central and eastern part of the Krkonose-Jizera Massif suggests that the country rocks to voluminous Cambrian-Ordovician magmatic bodies were largely eroded during the formation of early Palaeozoic rift basins alon
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2012
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Geological Magazine
ISSN
0016-7568
e-ISSN
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Volume of the periodical
149
Issue of the periodical within the volume
3
Country of publishing house
GB - UNITED KINGDOM
Number of pages
16
Pages from-to
443-458
UT code for WoS article
000302369600006
EID of the result in the Scopus database
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