Results 1 to 10 of about 193,636 (174)
Validating Structural Styles in the Flysch Basin Northern Rif (Morocco) by Means of Thermal Modeling
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).
Oriol Gimeno-Vives +2 more
exaly +3 more sources
Comprehension of the ophiolitic mélange plays a key role in the tectonic reconstruction of an ancient orogenic belt in terms of plate tectonics. The tectonic nature of the NNW‐trending southern Jinshajiang ophiolitic mélange is still controversial.
Di Xin +4 more
doaj +2 more sources
Investigation of recent catastrophic landslides in the flysch belt of Outer Western Carpathians (Czech Republic): progress towards better hazard assessment [PDF]
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.
Ivo Baron, Jan Klimeš
exaly +1 more source
Numerical analysis of deep-seated mass movements in the Magura Nappe; Flysch Belt of the Western Carpathians (Czech Republic) [PDF]
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 ...
Ivo Baron +2 more
exaly +1 more source
The Svecokarelian orogenic cycle and related metallogenesis in Finland [PDF]
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
Petrogenesis and evolution of an early Proterozoic collisional orogenic belt: The granulite belt of Lapland and the Belomorides (Fennoscandia) [PDF]
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 +1 more source
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
A positive gravity anomaly was observed in the Flysch belt realm. Based on this fact and available geological knowledge we suppose that the source of gravity anomaly might be carbonate rocks lying perhaps in the footwall of Flysch sediments.
Ľudovít KUCHARIČ +3 more
doaj +1 more source
Tectonics and gravitational phenomena (Nanos, Slovenia)
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
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

