A geophysical model of the Variscan orogenic root (Bohemian Massif):Implications for modern collisional orogens

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F11%3A10098785" target="_blank" >RIV/00216208:11310/11:10098785 - isvavai.cz</a>
Alternative codes found
RIV/00216208:11320/11:10098785
Result on the web
<a href="http://dx.doi.org/10.1016/j.lithos.2010.08.008" target="_blank" >http://dx.doi.org/10.1016/j.lithos.2010.08.008</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.lithos.2010.08.008" target="_blank" >10.1016/j.lithos.2010.08.008</a>

Result language
angličtina
Original language name
A geophysical model of the Variscan orogenic root (Bohemian Massif):Implications for modern collisional orogens
Original language description
A new model of the structure and composition of the Variscan crust inthe Bohemian Massif is proposed based on 3D gravity modelling, geological data, seismic refraction (CEL09) and reflection (9HR) sections. The Bohemian Massif crust is characterized by asuccession of positive and negative anomalies of about 6080 km wavelength for nearly constant Moho depths. The south-western part of the Bohemian Massif displays a large negative Bouguer anomaly corresponding to high grade rocks (granulites and migmatites) of the Palaeozoic crustal root represented by the Moldanubian domain.
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
DE - Earth magnetism, geodesy, geography
OECD FORD branch
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Project
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach

Publication year
2011
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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