Results 11 to 20 of about 7,213 (219)
An olistostrome–mélange belt formed along a suture: Bornova Flysch zone, western Turkey
Tectonophysics, 2012 Abstract The Bornova Flysch Zone (BFZ) in western Turkey is a regional olistostrome–melange belt located between the Izmir–Ankara Tethyan suture in northwest and the Menderes Massif in the southeast. The BFZ consists mostly of tectonized gravity mass flows.
Okay, Aral I. +4 more
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Stratigraphy, sedimentology and structure of the Numidian Flysch thrust belt in northern Tunisia
Journal of African Earth Sciences, 2010 Abstract The Oligo-Miocene Numidian Flysch of northern Tunisia has long been divided into three distinct lithostratigraphic units considered as vertically superimposed: the lower unit or the “Zouza member”, the middle unit or the “Kroumirie member” and the upper unit or the “Babouch member”.
Riahi Sami +6 more
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Sedimentary Geology, 1993 Abstract Various techniques of geometric and kinematic analyses, including cross-section balancing and forward modeling, have been applied successfully to the outer Carpathian flysch units along regional geologic profiles crossing the belt from its undeformed foreland to the Pieniny klippen belt (western Carpathians, Poland) or to the central east ...
F. Roure, E. Roca, W. Sassi
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The Svecokarelian orogenic cycle and related metallogenesis in Finland [PDF]
Bulletin of the Geological Society of Finland, 1975 General features of the Svecokarelian orogenic belt in Finland together with the ore deposits and their environments in the belt are reported. The sedimentary groups, igneous phases and ore deposits are considered functions of the orogeny.
T. Piirainen
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Field trip – Outer Flysch Carpathians and Pieniny Klippen Belt (PKB)
Geotourism/Geoturystyka, 2023 We are glad that we can meet personally during the 2nd Symposium of the IGCP 710 Project, after the pandemic time, which disrupted our idea of regular, annual meetings. After the 1st virtual meeting during the autumn of 2021, we have now the chance to discuss face to face and go to the field together to touch „Tethyan” rocks for a better understanding ...
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Petrogenesis and evolution of an early Proterozoic collisional orogenic belt: The granulite belt of Lapland and the Belomorides (Fennoscandia) [PDF]
Bulletin of the Geological Society of Finland, 1984 The tectonic and metamorphic pattern of the Precambrian crust exposed in the eastern Baltic Shield is characterized by two adjacent high-grade belts (Tana and Granulite belts) located between the Archean Inari-Kola craton to the east and the South ...
P. Barbey +4 more
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Validating Structural Styles in the Flysch Basin Northern Rif (Morocco) by Means of Thermal Modeling
Geosciences, 2020 Vitrinite reflectance and a micro-Raman spectroscopy parameters data set have been acquired on dispersed organic matter of the Maghrebian flysch basin and the Tangiers unit across a NE-SW section in the north-western Rif belt (North Morocco).
Achraf Atouabat +6 more
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Geologica Carpathica, 2019 The Vienna Basin is situated at the contact of the Bohemian Massif, Western Carpathians, and Eastern Alps. Deep borehole data and an existing magnetotelluric profile were used in density modelling of the pre-Neogene basement in the Slovak part of the ...
Šamajová Lenka +7 more
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Geological structure and evolution of the Pieniny Klippen Belt to the east of the Dunajec River : a new approach (Western Outer Carpathians, Poland) [PDF]
, 2014 The area studied, known as the Małe (Little) Pieniny Mts., belongs to the Pieniny Klippen Belt (PKB), a suture zone that separates the Central Carpathians from the Outer Carpathian accretionary wedge. Along its northern boundary the PKB is separated from
Oszczypko, Nestor +1 more
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Tectonics and gravitational phenomena (Nanos, Slovenia)
Geologija, 2021 The Istra Pushed Area is a specifically deformed territory of the northwestern part of the External Dinarides. It formed due to the movement of the Istra block as part of the Adriatic Microplate (Adria) towards the Dinarides since the middle Miocene ...
Ladislav PLACER +2 more
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