Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F12%3A00188578" target="_blank" >RIV/68407700:21110/12:00188578 - isvavai.cz</a>
Alternative codes found
RIV/00216208:11310/12:10128650 RIV/00025798:_____/12:00000098
Result on the web
<a href="http://dx.doi.org/10.1016/j.jsg.2011.12.011" target="_blank" >http://dx.doi.org/10.1016/j.jsg.2011.12.011</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.jsg.2011.12.011" target="_blank" >10.1016/j.jsg.2011.12.011</a>
Alternative languages
Result language
angličtina
Original language name
Magmatic to solid state fabrics in syntectonic granitoids recording early Carboniferous orogenic collapse in the Bohemian Massif
Original language description
The w354e336 Ma Central Bohemian Plutonic Complex is a Variscan magmatic arc that developed in the central Bohemian Massif in response to subduction of the Saxothuringian lithosphere beneath the Teplá eBarrandian microplate. Magmatic to solid state fabrics in the most voluminous portion of this arc (the w346 Ma Blatná pluton) record two superposed orogenic events: dextral transpression associated with arc-parallel stretching and arc-perpendicular shortening, and normal shearing associated with exhumation of the high-grade core of the orogen (Moldanubian unit). This kinematic switch is an important landmark in the evolution of this segment of the Variscan belt for it marks the cessation of subduction-related compressive forces in the upper crust givingway to gravity-driven normal move- ments of the TepláeBarrandian hanging wall block relative to the high-grade Moldanubian footwall. We use thermal modeling to demonstrate that the emplacement of huge volumes of arc magmas and their slow
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)
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
Journal of Structural Geology
ISSN
0191-8141
e-ISSN
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Volume of the periodical
36
Issue of the periodical within the volume
March
Country of publishing house
NL - THE KINGDOM OF THE NETHERLANDS
Number of pages
16
Pages from-to
27-42
UT code for WoS article
000301630600004
EID of the result in the Scopus database
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