Results 51 to 60 of about 259 (94)

Paleogene of the Magura Nappe adjacent to the Pieniny Klippen Belt between Szczawnica and Krościenko (Outer Carpathians, Poland)

Tyt. z nagłówka.Bibliogr. s. 373-375.The present authors investigated the Paleogene deposits of the internal zone of the Magura Basin known as the Krynica Subunit or Krynica zone in Poland.
Golonka, Jan
core  

Topography of the Magura floor thrust and morphotectonics of the Outer West Carpathians in Poland [PDF]

, 2008
Neotectonic (Pliocene-Quaternary) elevations and depressions detected on maps of subenvelope surfaces of the topography of the Outer West Carpathians of Poland are, to a certain extent, portrayed on the map showing topography of the Magura floor thrust ...
Oszczypko, Nestor, Oszczypko, N., Zuchiewicz, Witold, Zuchiewicz, W.   +3 more
core  

Mofetta from Tylicz in the Magura Nappe of the Outer Carpathians

, 2013
The described mofetta of CO2 is located in the Sądecki Beskid Mts, within the Poprad Landscape Park in Tylicz near Krynica, where it can be found on the SE slope of the Szalone hill, between the Syhowny and Bradowiec streams, the rightbank tributaries of
Rajchel, J., Cisek, J., Rajchel, L.
core  

Depositional architecture of the Magura Beds from the Siary zone, south of Gorlice (Magura Nappe, Polish Outer Carpathians)

, 2007
Detailedanalysis of lithofacies and their distribution in the Magura Beds in 11 transects in the eastern part of the Siary zone, revealed 16 facies and 6 associations of genetically and spatially related facies.
Warchoł, M.
core  

Exotic rocks of the Krynica Zone (Magura nappe) and their palaeogeographic significance [PDF]

, 2006
Poziomy egzotykowe w strefie krynickiej grupują się w utworach formacji szczawnickiej, zarzeckiej i magurskiej. Wśród egzotyków skał osadowych strefy krynickiej rozpoznano: pelagiczne wapienie tytonu-neokomu oraz litotamniowe wapienie paleogenu.
Oszczypko, Nestor, Oszczypko-Clowes, Marta, Oszczypko, N., Salata, D., Salata, Dorota, Oszczypko-Clowes, M.   +5 more
core  

Provenance analyses of the Late Cretaceous : Palaeocene deposits of the Magura Basin (Polish Western Carpathians) : evidence from the heavy minerals study

, 2005
The Late Cretaceous - Palaeocene sequence of the Magura Nappe in Poland is underlain by the Albian-Cenomanian spotty marls at the base and overlapped by the PalaeoccnelEarly Eocene variegated shales at the top. The spotty marls arc followed by variegated
Oszczypko, Nestor, Salata, Dorota
core  

Fossilized bioelectric wire - the trace fossil <i>Trichichnus</i>. [PDF]

Biogeosciences, 2015
Kędzierski M, Uchman A, Sawlowicz Z, Briguglio A.   +3 more
europepmc   +1 more source

Reconstruction of stress directions in the Magura and Silesian Nappes (Polish Outer Carpathians) based on analysis of regional folds

, 2003
Statistic analysis of the bed orientation in the Magura and Silesian Nappes was performed in order to establish the directions of regional fold axes. On this ground, variations of the main horizontal stress directions were inferred for both nappes.
Szczęsny, R.
core  

Evaluating the applicability of MESS (matrix exponential spatial specification) model to assess water quality using GIS technique in agricultural mountain catchment (Western Carpathian). [PDF]

Environ Monit Assess, 2018
Halecki W, Stachura T, Fudała W, Rusnak M.   +3 more
europepmc   +1 more source

Biostratigraphic and paleoecologic interpretation of the agglutinated foraminifera assemblages of the Paleocene-Middle Eocene deposits of the Magura Nappe in the area of Sucha Beskidzka (Outer Carpathians) [PDF]

, 2000
Analiza otwornic aglutynujących z paleoceńsko-środkowoeoceńskich osadów płaszczowiny magurskiej, ze strefy raczańskiej północnej, była przedmiotem badań, na podstawie których ustalono, że wyższa część warstw inoęeramowych, pstre lupki dolne z Łabowej ...
Waśkowska-Oliwa, Anna
core