Results 51 to 60 of about 1,578 (175)

Paleopiezometry – the new investigation method applied to the Penninic suture zone in comparison to the Meliata-Hallstatt suture zone [PDF]

Acta Montanistica Slovaca, 2016
The method of paleopiezometry reveals new pleopiezometric data of differential stresses within the calcite veins in outcrops with developed fold structure near the village of Chmeľnica – eastern sector of the Pieniny Klippen Belt – PKB(the Inner ...
Barbora Zákršmidová, Stanislav Jacko, Zoltan Németh   +2 more
doaj   +1 more source

Výskyt spodnokriedových magmatických hornín medzi Podbrančom a Myjavou [PDF]

Geologické práce. Správy, 2020
Occurrences of magmatic rocks were identifid north of the settlement Belanskovci (part of Myjava town), on the ridge of the elevation point 464 m a. s. l. east of the settlement Podzámok (part of the Podbranč village).
Tamás Csibri, Dušan Plašienka, Rastislav Demko   +2 more
doaj  

Geological setting and lithological inventory of the Czarna Woda conglomerates (Magura Nappe, Polish Outer Carpathians) [PDF]

, 2020
During the late Oligocene to early Miocene the residual Magura Basin was located along the front of the Pieniny Klippen Belt (PKB). This basin was supplied with clastic material derived from a south-eastern direction. In the Małe (Little) Pieniny Mts. in
Olszewska, Barbara, Oszczypko, Nestor, Oszczypko-Clowes, Marta   +2 more
core   +1 more source

A unique Valanginian paleoenvironment at an iron ore deposit near Zengővárkony (Mecsek Mts, South Hungary), and a possible genetic model [PDF]

, 2007
The spatially restricted Early Valanginian iron ore (limonite) and manganese deposit at Zengõvárkony (Mecsek Mts, southern Hungary) contains a rich, strongly limonitized, remarkably large-sized (specimens are 30–70% larger than those at their type ...
Abed-Navandi D., Abed-Navandi D., Bilik I., Bilik I., Bujtor L., Bércziné Makk A., Bércziné Makk A., Callender W.R., Campbell K.A., Campbell K.A., Campbell K.A., Campbell K.A., Császár G., Dover C.L., Dover C.L., Fõzy I., Golonka J., Haas J., Harangi Sz., Harangi Sz., Jannasch H.W., Juhász, Kolosváry G., Kovács S., Krobicki M., Krobicki M., Little C.T.S., Little C.T.S., László Bujtor, Molnár J., Mullineaux L., Nagy I., Nekvasilová O., Nekvasilová O., Palik P., Pantó G., Pantó G., Pohl M.E., Spötl Ch., Sztrókay K., Szörényi E., Szörényi E., Wein Gy.   +42 more
core   +1 more source

The Middle Jurassic succession in the central sector of the Pieniny Klippen Belt (Sprzycne Creek): implications for the timing of the Czorsztyn Ridge development

Geologica Carpathica, 2015
In this study, we revisit the stratigraphic age and discuss sedimentary characteristics of the lower Middle Jurassic turbidite deposits (“black flysch”) of the Szlachtowa Formation, as well as the under- and overlying members of the Sprzycne Creek ...
Segit Tomasz, Matyja Bronisław A., Wierzbowski Andrzej   +2 more
doaj   +1 more source

Where was the Magura Ocean? [PDF]

, 2015
In the Late Jurassic to Early Cretaceous palaeogeography of the Alpine Tethys the term Ocean is used for different parts of these sedimentary areas: eg. Ligurian-Piedmont and Penninic, Magura, Pieniny, Valais and Ceahlau-Severins oceans. The Magura Ocean
Olszewska, Barbara, Oszczypko, Nestor, Oszczypko-Clowes, Marta, Ślączka, Andrzej   +3 more
core   +1 more source

Microfacies and geochemistry of Kimmeridgian limestone strata in the Eastern Pontides (North‐East Turkey): Palaeoclimate and palaeoenvironmental influence on organic matter enrichment

The Depositional Record, Volume 11, Issue 1, Page 4-21, February 2025.
Kimmeridgian limestone (KL) strata are one best example of a peritidal carbonate that records palaeogeographic and palaeoclimate conditions in Eastern Pontide, Eastern Black Sea region. The KL strata are represented by well‐preserved dark grey lime‐mudstones that archive important geochemical proxy.
Merve Özyurt, M. Ziya Kırmacı
wiley   +1 more source

Tectono-sedimentary analysis using the anisotropy of magnetic susceptibility: a study of the terrestrial and freshwater Neogene of the Orava Basin

Geologica Carpathica, 2017
The Orava Basin is an intramontane depression filled with presumably fine-grained sediments deposited in river, floodplain, swamp and lake settings. The basin infilling constitutes a crucial record of the neoalpine evolution of the Inner/Outer Carpathian
Łoziński Maciej, Ziółkowski Piotr, Wysocka Anna   +2 more
doaj   +1 more source

Age, Kinematic and Thermal Constraints of Syn‐Orogenic Low‐Temperature Deformation Events: Insights From Thermochronology and Structural Data of the Nekézseny Thrust (Alpine‐Carpathian‐Dinaric Area)

Tectonics, Volume 43, Issue 4, April 2024.
Abstract Unraveling the age and kinematics of low temperature deformation events is crucial in understanding the late‐stage evolution of orogens. However, accurate age constraints can often be challenging to obtain due to unideal outcrop conditions, large sedimentary hiatuses or the lack of well‐defined thermal events.
Éva Oravecz, Zsolt Benkó, Róbert Arató, István Dunkl, Gábor Héja, Szilvia Kövér, Tibor Németh, László Fodor   +7 more
wiley   +1 more source

Middle Jurassic stromatactis mud-mound in the Pieniny Klippen Belt (Western Carpathians)

Facies, 2002
A stromatactis mud-mound has been found near SlavnickeŽ Podhorie in the Czorsztyn Unit of the Pieniny Klippen Belt (Western Carpathians, Slovakia). Its stratigraphic range is Bathonian to Callovian and it is one of the youngest known true stromatactis mud-mounds.
Aubrecht, Roman, Szulc, Joachim, Michalik, Jozef, Schlögl, Ján, Wagreich, Michael   +4 more
openaire   +3 more sources