Results 91 to 100 of about 831 (199)

The Babín Klippen – a peculiar branch of the Orava sector of the Pieniny Klippen Belt (Slovakia)

open access: yesMineralia Slovaca
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
doaj   +1 more source

Diagenetic history of the Podhale flysch basin

open access: yes, 2018
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
core   +1 more source

The position and age of flysch deposits in the Crimean Mountains (Southern Ukraine) [PDF]

open access: yes, 2017
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
core   +1 more source

JURASSIC PALEOGEOGRAPHY OF THE PIENINY AND OUTER CARPATHIAN BASINS

open access: yesRivista Italiana di Paleontologia e Stratigrafia, 2004
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

Geochemistry and Nd isotopic composition of the Early Paleozoic flysch sequence in the Chinese Altai, Central Asia: evidence for a northward-derived mafic source and insight into Nd model ages in accretionary orogen

open access: yes, 2012
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
core   +1 more source

Geology of the Ordovician rocks between Leadhills and Abington, Lanarkshire

open access: yes, 2015
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.
core  

Kinematic evolution of the eastern Tethyan Himalaya: Constraints from magnetic fabric and structural properties of the Triassic flysch in SE Tibet

open access: yes, 2011
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
core   +1 more source

European provenance of the Numidian Flysch in northern Tunisia

open access: yes, 2010
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
core   +1 more source

Field trip - Outer Flysch Carpathians, Pieniny Klippen Belt (PKB), and Tatra Mountains

open access: yesGeotourism/Geoturystyka
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

From Flysch to Molasse - sedimentary and tectonic evolution of late Caledonian - early Hercynian Foreland Basin in North Qilian Mountains

open access: yes, 2003
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
core  

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