Numerical analysis of deep-seated mass movements in the Magura Nappe; Flysch Belt of the Western Carpathians (Czech Republic) [PDF]
Natural Hazards and Earth System Sciences, 2005 Deep-seated slope failures are common features in the mountains of the Raca Unit, Magura Nappe of the Flysch Belt of Western Carpathians. Since they represent very complicated system, understanding of their evolution and triggers still remains unclear ...
I. Baron +4 more
doaj +7 more sources
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
doaj +2 more sources
Structure and dynamics of deep-seated slope failures in the Magura Flysch Nappe, outer Western Carpathians (Czech Republic) [PDF]
Natural Hazards and Earth System Sciences, 2004 Deep-seated mass movements currently comprise one of the main morphogenetic processes in the Flysch Belt of the Western Carpathians of Central Europe. These mass movements result in a large spectrum of slope failures, depending on the type of movement ...
I. Baron +5 more
doaj +1 more source
The onset of flysch sedimentation in the Kaoko Belt (NW Namibia) – Implications for the pre-collisional evolution of the Kaoko–Dom Feliciano–Gariep orogen [PDF]
Precambrian Research, 2017 Abstract Detrital zircon provenance study of a metamorphosed sedimentary succession in the eastern part of the Kaoko Belt in Namibia has revealed two distinct sources for the Neoproterozoic sedimentation along the southwestern Congo Craton margin. The lower part of the succession shows detrital zircon ages consistent with erosion of Paleoproterozoic ...
Jiří Konopasek +2 more
exaly +5 more sources
Investigation of recent catastrophic landslides in the flysch belt of Outer Western Carpathians (Czech Republic): progress towards better hazard assessment [PDF]
Natural Hazards and Earth System Sciences, 2009 Rapid snow melting and intense precipitation triggered and reactivated tens of mostly shallow landslides in the eastern part of the Czech Republic at the turn of March and April 2006.
J. Klimeš +6 more
doaj +4 more sources
Connecting the late Neoproterozoic flysch sedimentation in the Gariep Belt (Namibia) with its potential source region in southern Dom Feliciano Belt (Uruguay) – a U-Pb detrital and protolith zircon study. [PDF]
, 2020 The Dom Feliciano Belt in Uruguay represents a counterpart of the Gariep Belt in Namibia and these two belts are presently considered as relics of one orogen split by the Atlantic Ocean. In this study, two presumed flysch samples from the Marmora Terrane of the Gariep Belt in Namibia, and five samples from potential source areas in the Nico Perez ...
Gilberg, Ina Nordbø
openaire +2 more sources
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
doaj +1 more source
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
doaj +1 more source
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
doaj +1 more source
Геодинамика и тектонофизика, 2017 Tectonic-magmatic reworking of accretionary wedges is a key process responsible for differentiation and stabilization of continental crustal in accretionary orogens. This generic problem can be exemplified by magmatic evolution of the Chinese Altai which
Yingde Jiang +7 more
doaj +1 more source