Late Cretaceous and Cenozoic dynamics of the Bohemian Massif inferred from the paleostress history of the Lusatian Fault Belt

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F15%3A00443496" target="_blank" >RIV/67985831:_____/15:00443496 - isvavai.cz</a>
Alternative codes found
RIV/67985891:_____/15:00443496
Result on the web
<a href="http://dx.doi.org/10.1016/j.jog.2015.02.006" target="_blank" >http://dx.doi.org/10.1016/j.jog.2015.02.006</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.jog.2015.02.006" target="_blank" >10.1016/j.jog.2015.02.006</a>

Result language
angličtina
Original language name
Late Cretaceous and Cenozoic dynamics of the Bohemian Massif inferred from the paleostress history of the Lusatian Fault Belt
Original language description
An analysis of fault-slip data from the Lusatian Fault Belt, limiting the Lusatian Block of the Bohemian Massif in the SW, yielded parameters of eight successive paleostress patterns, Late Cretaceous to Plio-Pleistocene in age. These patterns were linkedwith specific stages in fault kinematics and fault-belt deformation. They include (1) ?1, NE- to NNE-directed compression in a reverse fault regime (?3 vertical) associated with major thrusting and drag zone formation in the latest Cretaceous, precededby pre-drag origin of deformation bands ?0; (2) ??1-2, WNW-directed extension associated with emplacement of polzenite-group volcanics (ca 80-61Ma) and influx of hydrothermal fluids, overlapping in time with ?1; (3) ?2, N-directed compression in a reverse fault regime, probably Paleocene in age, associated with thrusting and intensive shear faulting in adjacent parts of blocks; (4) ??3, Early Oligocene W- to WNW-directed extension in a regime of strike-slip faulting (?2 vertical), probab
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
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Project
<a href="/en/project/GAP210%2F12%2F0573" target="_blank" >GAP210/12/0573: Late Quaternary seismogenic faulting and evolution of fault-controlled sedimentary basins in the eastern Bohemian Massif</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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