Results 51 to 60 of about 639 (105)

Mélanges and broken formations at the boundary zone of the Magura and Silesian nappes (Gorlice area, Polish Outer Carpathians) : a result of sedimentary and tectonic processes [PDF]

open access: yes, 2014
Based on geological field mapping, analyses of cores from explanatory wells, and foraminiferal age control data, we have differentiated a few types of mélanges and broken formations at the bordering zone between the Magura and Silesian nappes (Gorlice ...
Malata, Ewa   +3 more
core   +1 more source

The stratigraphy of the Ropa tectonic window (Magura Nappe, Western Carpathians, Poland) [PDF]

open access: yes, 2008
The Ropa tectonic window of the Magura Nappe is composed of Oligocene deposits that belong to the Grybów Nappe. The youn gest depos its of the Ropa tectonic window are correlated with calcareous nannoplanton zones NP24 and NP25.
Oszczypko-Clowes, Marta
core  

The genesis of the carbon dioxide in the Polish Outer Carpathians : Szczawa tectonic window case study : new insight [PDF]

open access: yes, 2018
In the Polish sector of the Magura Nappe have long been known and exploited carbonate mineral waters, saturated with carbon dioxide, known as the "shchava (szczawa)".
Oszczypko, Nestor   +2 more
core   +1 more source

Geoturystyczna ścieżka rowerowa wokół Nowego Targu (Karpaty, Polska) [PDF]

open access: yes, 2020
The area in the vicinity of Nowy Targ is located within the northern part of the Orawa-Nowy Targ Basin and the southern slopes of the Gorce Mountains in the Polish sector of the Outer Carpathians. Geologically, the region is built of the Upper Cretaceous–
Chodyń, Rafał   +3 more
core   +1 more source

The comparison of anisotropy of magnetic remanence with the anisotropy of magnetic susceptibility of the Dukla nappe from the Outer Western Carpathians [PDF]

open access: yes, 2014
The Carpathians belong to the European Alpine system, which was formed during the convergence and collision of the European and African plates. The Polish segment of the Western Outer Carpathians is a north-verging thrust-and-fold belt composed largely ...
Kiss, Dániel   +2 more
core  

The role of compressional tectonics, sedimentary transport and mineral composition on AMS and AARM fabrics. A case study of the flysch from the Dukla nappe, OuterWestern Carpatians, Poland [PDF]

open access: yes, 2015
The Carpathians belong to the European Alpine system. The Polish segment of the Western Outer Carpathians is a north-verging thrust-and-fold belt composed largely of Lower Cretaceous to Lower Miocene flysch.
Kiss, Dániel   +2 more
core  

Geoturystyczne walory Gorczańskiego Parku Narodowego i jego otoczenia (Karpaty Zewnętrzne, Polska) [PDF]

open access: yes, 2016
The Gorce Mountains are a picturesque range in the Polish sector of the Outer Carpathians. They are built with turbiditic deposits, representing sedimentary successions of the Krynica and Bystrica Subunits of the Magura Nappe, Late Cretaceous- Paleogene ...
Chodyń, Rafał   +3 more
core   +1 more source

Collision with Gondwana or with Baltica? Ordovician magmatic arc volcanism in the Marmarosh Massif (Eastern Carpathians, Ukraine). [PDF]

open access: yesInt J Earth Sci, 2022
Gawęda A   +8 more
europepmc   +1 more source

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