International audienceNumerous talc, magnesite and siderite ore deposits occur in the Central Western Carpathians (Slovakia) along theso-called Gemer-Vepor Contact Zone, which marks the contact between two major blocks of Variscan basement,the Vepor and Gemer units. During the polyphase deformation of Cretaceous age, the Gemer Unit was first thrustover the Vepor Unit. This is well documented by the development of subhorizontal and prograde metamorphic foliationreaching up to amphibolite facies conditions in the Vepor and by the development of subvertical greenschistfacies cleavages in the Gemer Unit. The subsequent exhumation of the Vepor Unit along large-scale detachmentzone is documented by the development of subhorizontal lower grade cle...
This work is primarily focused on the interpretation of leuco-cratic granite emplaced along the boun...
The Tux-Lanersbach magnesite-scheelite deposit is one of several small strata-bound scheelite deposi...
International audienceWe describe, date and constrain the PT conditions of a syntectonic inverted m...
International audienceNumerous talc, magnesite and siderite ore deposits occur in the Central Wester...
The studied area extends from the Ochtiná Unit in Western Carpathians to the Veitsch Nappe Eastern A...
Strong tectonic remobilisation and shear zone development are typical features of the easternmost pa...
International audienceThe Ochtiná Unit is situated in the ENE-WSW-trending contact zone between two ...
International audienceSodic metasomatites (albitites) occur around and within siderite veins in the ...
NW-SE faults has plaged a decisive role in the Alpine development of the eastern margin of the Wes-t...
Three small bodies of amphibolites and associated graphitic gneisses from the Suchý and Malá Magura ...
ly orthogneises and metasediments, there are Carboniferous (U)HP rocks forming small dispersed eclog...
Abstract: Internal sectors of the Alpine-Balkan-Carpathian-Dinaride (ABCD) orogen comprise fundament...
Metamorphic basement of the Pannonian Basin consists of blocks of incompatible metamorphic and struc...
Western Carpathians are characteristic for their complicated geological structure and uncertain tect...
International audienceThe South Armorican Shear Zone (SASZ), in the French Armorican Variscan belt, ...
This work is primarily focused on the interpretation of leuco-cratic granite emplaced along the boun...
The Tux-Lanersbach magnesite-scheelite deposit is one of several small strata-bound scheelite deposi...
International audienceWe describe, date and constrain the PT conditions of a syntectonic inverted m...
International audienceNumerous talc, magnesite and siderite ore deposits occur in the Central Wester...
The studied area extends from the Ochtiná Unit in Western Carpathians to the Veitsch Nappe Eastern A...
Strong tectonic remobilisation and shear zone development are typical features of the easternmost pa...
International audienceThe Ochtiná Unit is situated in the ENE-WSW-trending contact zone between two ...
International audienceSodic metasomatites (albitites) occur around and within siderite veins in the ...
NW-SE faults has plaged a decisive role in the Alpine development of the eastern margin of the Wes-t...
Three small bodies of amphibolites and associated graphitic gneisses from the Suchý and Malá Magura ...
ly orthogneises and metasediments, there are Carboniferous (U)HP rocks forming small dispersed eclog...
Abstract: Internal sectors of the Alpine-Balkan-Carpathian-Dinaride (ABCD) orogen comprise fundament...
Metamorphic basement of the Pannonian Basin consists of blocks of incompatible metamorphic and struc...
Western Carpathians are characteristic for their complicated geological structure and uncertain tect...
International audienceThe South Armorican Shear Zone (SASZ), in the French Armorican Variscan belt, ...
This work is primarily focused on the interpretation of leuco-cratic granite emplaced along the boun...
The Tux-Lanersbach magnesite-scheelite deposit is one of several small strata-bound scheelite deposi...
International audienceWe describe, date and constrain the PT conditions of a syntectonic inverted m...