Formation of elongated granite-migmatite domes as isostatic accommodation structures in collisional orogens
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10283110" target="_blank" >RIV/00216208:11310/14:10283110 - isvavai.cz</a>
Alternative codes found
RIV/67985530:_____/14:00425801 RIV/00025798:_____/14:00000032
Result on the web
<a href="http://dx.doi.org/10.1016/j.jog.2013.10.002" target="_blank" >http://dx.doi.org/10.1016/j.jog.2013.10.002</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.jog.2013.10.002" target="_blank" >10.1016/j.jog.2013.10.002</a>
Alternative languages
Result language
angličtina
Original language name
Formation of elongated granite-migmatite domes as isostatic accommodation structures in collisional orogens
Original language description
The mid-Carboniferous Pelhrimov core complex, Bohemian Massif, is a crustal-scale elongated granite-migmatite dome interpreted to have formed by gravity-driven diapiric upwelling of the metapelitic middle crust. The vertical diapiric flow is evidenced byoutward-dipping foliation and lineation patterns, deformation coeval with the widespread presence of melt, rapid exhumation of the dome center from depths corresponding to pressure of about 0.6 GPa to shallow levels (pressure less than 0.2 GPa) within 2M.y., and kinematic indicators of downward return flow of the mantling rocks. As compared to common diapirs, however, the Pelhrimov complex exhibits a more complicated inferred strain pattern with two perpendicular, irregularly alternating directions ofhorizontal extension in what is interpreted as the diapir head. Comparison of structural data from migmatites with anisotropy of magnetic susceptibility (AMS) data in granites also reveals that only final increments of strain are recorde
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
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2014
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 Geodynamics
ISSN
0264-3707
e-ISSN
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Volume of the periodical
73
Issue of the periodical within the volume
leden
Country of publishing house
GB - UNITED KINGDOM
Number of pages
18
Pages from-to
100-117
UT code for WoS article
000336235900009
EID of the result in the Scopus database
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