Behaviour of geochronometers and timing of metamorphic reactions during deformation at lower crustal conditions: phase equilibrium modelling and U-Pb dating of zircon, monazite, rutile and titanite from the Kalak Nappe Complex, northern Norway
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10297516" target="_blank" >RIV/00216208:11310/15:10297516 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1111/jmg.12131" target="_blank" >http://dx.doi.org/10.1111/jmg.12131</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1111/jmg.12131" target="_blank" >10.1111/jmg.12131</a>
Alternative languages
Result language
angličtina
Original language name
Behaviour of geochronometers and timing of metamorphic reactions during deformation at lower crustal conditions: phase equilibrium modelling and U-Pb dating of zircon, monazite, rutile and titanite from the Kalak Nappe Complex, northern Norway
Original language description
This study investigates the behaviour of the geochronometers zircon, monazite, rutile and titanite in polyphase lower crustal rocks of the Kalak Nappe Complex, northern Norway. A pressure-temperature-time-deformation path is constructed by combining microstructural observations with P-T conditions derived from phase equilibrium modelling and U-Pb dating. The following tectonometamorphic evolution is deduced: A subvertical S1 fabric formed at similar to 730-775 degrees C and similar to 6.3-9.8kbar, abovethe wet solidus in the sillimanite and kyanite stability fields. The event is dated at 702 +/- 5Ma by high-U zircon in a leucosome. The S1 fabric was overprinted by a subhorizontal S2 fabric, which formed at similar to 600-660 degrees C and similar to 10-12kbar. Rutile that originally grew during the S1-forming event lost its Zr-in-rutile and U-Pb signatures during the S2-forming event. It records Zr-in-rutile temperatures of 550-660 degrees C and Caledonian ages of 440-420Ma. Titanite
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
<a href="/en/project/GA14-25995S" target="_blank" >GA14-25995S: Tracking magmas from source to pluton: new insight into granites diversity</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2015
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of Metamorphic Geology
ISSN
0263-4929
e-ISSN
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Volume of the periodical
33
Issue of the periodical within the volume
5
Country of publishing house
GB - UNITED KINGDOM
Number of pages
22
Pages from-to
513-534
UT code for WoS article
000355742300004
EID of the result in the Scopus database
2-s2.0-84930378565