Results 91 to 100 of about 831 (199)
The Babín Klippen – a peculiar branch of the Orava sector of the Pieniny Klippen Belt (Slovakia)
The Pieniny Klippen Belt (PKB) is a narrow, approx. 5 – 8 km wide zone at the boundary of the External and Internal Western Carpathians. The zone of the Babín Klippen, which is the main subject of this study, represents northerly situated branch of the ...
František Teťák +2 more
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Diagenetic history of the Podhale flysch basin
This text presents a one day field trip starting and ending in Zakopane, Poland, devoted to explaining geological history of the Tertiary flysch basin of Podhale, situated between the Tatra Mts. and the Pieniny Klippen Belt.
Środoń, Jan
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The position and age of flysch deposits in the Crimean Mountains (Southern Ukraine) [PDF]
The Crimean Mountains (CM) are regarded as part of the Alpine-Himalaya orogenic belt related to the collision of the Eurasian and African plates. Our research in the CM has allowed confirming the existence of at least two flysch formations of different ...
Oszczypko, Nestor +14 more
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JURASSIC PALEOGEOGRAPHY OF THE PIENINY AND OUTER CARPATHIAN BASINS
The Jurassic history of the Pieniny/Outer Carpathian basins reflects the evolution of the Circum-Tethyan area, especially its Alpine Tethys part. The Alpine Tethys that is Ligurian, Penninic Oceans and Pieniny/Magura Basin constitute the extension of the
JAN GOLONKA, MICHAL KROBICKI
doaj +1 more source
Although Nd isotopic composition of sedimentary rocks is considered as a useful tool to trace the provenance, their Nd model age (T DM) is usually misused to discuss the timing of crustal formation in accretionary orogen.
Chao Yuan +20 more
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Geology of the Ordovician rocks between Leadhills and Abington, Lanarkshire
NE-SW faults in the Abington area of the Northern Belt of the Southern Uplands define blocks up to 3.2 km wide. The strata, folded and locally overturned, young predominantly to the NW but blocks to the SW contain younger sequences.
Hepworth, Barry C.
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Anisotropy of magnetic susceptibility (AMS) combined with structural analysis are used in this work with the aim to characterize the tectonic evolution of the Triassic flysch within the eastern Tethyan Himalaya Thrust Belt in SE Tibet.
APPEL E. +6 more
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European provenance of the Numidian Flysch in northern Tunisia
The ultimate source of the deepwater Numidian Flysch sediments has long been a matter of controversy. Did the sediments of this late Cenozoic orogenic belt in the western Mediterranean derive from a European or African source, or from a combination of ...
Patel, Urval +13 more
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Field trip - Outer Flysch Carpathians, Pieniny Klippen Belt (PKB), and Tatra Mountains
The 36th HKT Workshop (Himalaya-Karakorum- Tibet) is organised by the AGH University of Krakow, Poland. Kraków is situated at the front of the Carpathian orogenic system of the ancient Tethys Ocean and is perfect place for meeting between European-Asian Alpine-Himalayan orogenic belt with long history of the Western and Eastern Tethyan Ocean Realms ...
openaire +1 more source
The Late Caledonian to Early Hercynian North Qilian orogenic belt in northwestern China is an elongate tectonic unit situated between the North China plate in the north and the Qaidam plate in the south.
Y Du (6951416) +3 more
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