Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Edyta Jurewicz"'
Autor:
Edyta Jurewicz, Paweł Karnkowski, Anna Czarnecka‐Skwarek, Emilia Wójcik, Ireneusz Gawriuczenkow
Publikováno v:
Earth Surface Processes and Landforms.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d40b3a9d985bd170333435cbeeaf0e34
https://doi.org/10.1002/esp.5609
https://doi.org/10.1002/esp.5609
Publikováno v:
Journal of the Geological Society. 178
We appreciate the attempts of Marzec et al. (2019) to investigate the geological structure of the Pieniny Klippen Belt (PKB) by means of seismic-reflection profiling, but in our opinion the authors’ main conclusions contradict the results of previo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4378916f99d07ceeacee40f1011bdc4f
https://doi.org/10.1144/jgs2020-021
https://doi.org/10.1144/jgs2020-021
Publikováno v:
European Journal of Mineralogy. 30:135-147
The occurrence of chevkinite-group minerals (CGM), zirconolite and Nb-rich ilmenite is reported in Miocene high-K trachyandesites from the Uherský Brod area, Czech Republic, their occurrence reflecting the high Nb and Zr abundances in the host rocks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e39349eddac5cafa1f831060954dd825
https://doi.org/10.1127/ejm/2017/0029-2693
https://doi.org/10.1127/ejm/2017/0029-2693
Autor:
Edyta Jurewicz
Publikováno v:
Swiss Journal of Geosciences. 111:245-267
The Pieniny Klippen Belt (PKB) is a narrow structure delineating the boundary between the Central and Outer Carpathians. It is built of nappes stacked during the Cretaceous and Paleocene and then re-folded in the Miocene during the formation of the O
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eebcf5f05eb65d06cf289b0d94d9b37c
https://doi.org/10.1007/s00015-017-0297-9
https://doi.org/10.1007/s00015-017-0297-9
Autor:
Magdalena Dąbrowska, Edyta Jurewicz
Publikováno v:
Acta Geologica Polonica. 63:137-151
63 Abstract Dąbrowska, M. and Jurewicz, E. 2013. Character and structural evolution of the Mała Łąka Fault in the Tatra Mts., Carpathians, Poland. Acta Geologica Polonica, (1), 137-151. Warszawa. The Mała Łąka Fault in the Tatra Mts. is a syns
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6052ba290623e84b2a76f7d93f64fb48
https://doi.org/10.2478/agp-2013-0005
https://doi.org/10.2478/agp-2013-0005
Publikováno v:
Lithos. :34-47
Miocene igneous rocks of the Western Outer Carpathians in Poland and Moravia, Czech Republic, were emplaced in a tectonic setting transitional between the European foreland and the Carpathian–Pannonian arc system. They form medium- to high-K calc-a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::470a61787390814b5babc8feb4033c60
https://doi.org/10.1016/j.lithos.2012.04.026
https://doi.org/10.1016/j.lithos.2012.04.026
Autor:
Urszula Stępień, Edyta Jurewicz
Publikováno v:
Geological Quarterly. 56:181-186
The Variscan orogeny of NE–SW compression has folded the Paleozoic core of the Holy Cross Mountains (Central Poland). The Checiny Anticline, formed during this tectonic event, is located in the southwestern part of the Kielce Unit. This paper prese
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5079534f29ece3b3cb66c37a3d75fcd5
https://doi.org/10.7306/gq.1069
https://doi.org/10.7306/gq.1069
Autor:
Tomasz Segit, Edyta Jurewicz
Publikováno v:
Geology, Geophysics & Environment. 44:127
The Pieniny Klippen Belt is a narrow, complex structure stretching along a tectonic boundary between the Central and Outer Carpathians. Its formation involved two main evolutionary stages, the first, related to Late Cretaceous-Paleocene folding and t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ff0de6aad93a6a574f4b4eaa7f4abc38
https://doi.org/10.7494/geol.2018.44.1.127
https://doi.org/10.7494/geol.2018.44.1.127