P-T-t-D record of crustal-scale horizontal flow and magma-assisted doming in the SW Mongolian Altai

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10298027" target="_blank" >RIV/00216208:11310/15:10298027 - isvavai.cz</a>
Alternative codes found
RIV/00025798:_____/15:00000022
Result on the web
<a href="http://dx.doi.org/10.1111/jmg.12124" target="_blank" >http://dx.doi.org/10.1111/jmg.12124</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1111/jmg.12124" target="_blank" >10.1111/jmg.12124</a>

Result language
angličtina
Original language name
P-T-t-D record of crustal-scale horizontal flow and magma-assisted doming in the SW Mongolian Altai
Original language description
The Chandman massif, a typical structure of the Mongolian Altai, consists of a migmatite-magmatite core rimmed by a lower grade metamorphic envelope of andalusite and cordierite-bearing schists. Theoldest structure in the migmatite-magmatite core is a subhorizontal migmatitic foliation S1 parallel to rare granitoid sills. This fabric is folded by upright folds F2 and transposed into a vertical migmatitic foliation S2 that is syn-tectonic, with up to several tens of metres thick granitoid sills.
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
—

Project
<a href="/en/project/GAP210%2F12%2F2205" target="_blank" >GAP210/12/2205: Crustal growth and construction of continental crust exemplified by Central Asian Orogenic Belt</a><br>
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year
2015
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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