The seismogenic pseudotachylytes from the Tribeč Mountains (Western Carpathians, Slovakia) were dated by means of the laser microprobe 40Ar/39Ar method. The Tribeč Mountain crystalline basement was buried to 5–7.5-km depths, where it experienced approximately >110°C and <210°C thermal conditions. The dated pseudotachylytes have spot ages between 58 ± 1 and 46 ± 1 Ma with a weighted mean age of 49.7 ± 1.3 Ma, indicating that seismic activity caused their origin, the propagation of subvertical basement marginal faults, and/or the inception of basement unroofing processes in the southern part of the Central Carpathian Paleogene Basin. The extensional tectonics were responsible for the exhumation of basement highs and the opening of the intramo...
Understanding the tectonic evolution of orogenic belts and intracratonic areas depends on our abilit...
The Tatric crystalline unit of the Western Carpathians in northern Slovakia displays an inverted met...
International audienceThe age of intraplate volcanism in northern Pannonian Basin of Carpathians is ...
Pre-Mesozoic exotic crystalline blocks within the Outer Carpathian flysch have potential to unravel ...
1] The Kyrgyz Range, the northernmost portion of the Kyrgyzstan Tien Shan, displays topographic evid...
A combination of four thermochronometers [zircon fission track (ZFT), zircon (U–Th)/He (ZHe), apatit...
The Kyrgyz Range, the northernmost portion of the Kyrgyzstan Tien Shan, displays topographic evidenc...
Detailed cathodoluminescence (CL) imaging of zircon crystals, coupled with Laser Abla-tion Multi-Col...
The tectonothermal evolution of the highest mountain range in the Carpathian arc—the Tatra Mountains...
This study tests alternative models for the growth of the Tatry Mountains (Central Western Carpathia...
[1] UV and CO2 laser-probe 40Ar/39Ar in situ analyses of phlogopite and muscovite in fibrous strain ...
We investigate the influence of unmelted clasts on the 40 Ar\\ 39 Ar age record of a Miocene pseudota...
The exhumation history of mountain belts can be derived from radiometric dating of detrital mineral ...
Tectono-thermal evolution of the northern part of Central Western Carpathians (Slovakia) was reveale...
International audienceThe Inner Carpathians comprise several distinct Neogene late-stage orogenic Pb...
Understanding the tectonic evolution of orogenic belts and intracratonic areas depends on our abilit...
The Tatric crystalline unit of the Western Carpathians in northern Slovakia displays an inverted met...
International audienceThe age of intraplate volcanism in northern Pannonian Basin of Carpathians is ...
Pre-Mesozoic exotic crystalline blocks within the Outer Carpathian flysch have potential to unravel ...
1] The Kyrgyz Range, the northernmost portion of the Kyrgyzstan Tien Shan, displays topographic evid...
A combination of four thermochronometers [zircon fission track (ZFT), zircon (U–Th)/He (ZHe), apatit...
The Kyrgyz Range, the northernmost portion of the Kyrgyzstan Tien Shan, displays topographic evidenc...
Detailed cathodoluminescence (CL) imaging of zircon crystals, coupled with Laser Abla-tion Multi-Col...
The tectonothermal evolution of the highest mountain range in the Carpathian arc—the Tatra Mountains...
This study tests alternative models for the growth of the Tatry Mountains (Central Western Carpathia...
[1] UV and CO2 laser-probe 40Ar/39Ar in situ analyses of phlogopite and muscovite in fibrous strain ...
We investigate the influence of unmelted clasts on the 40 Ar\\ 39 Ar age record of a Miocene pseudota...
The exhumation history of mountain belts can be derived from radiometric dating of detrital mineral ...
Tectono-thermal evolution of the northern part of Central Western Carpathians (Slovakia) was reveale...
International audienceThe Inner Carpathians comprise several distinct Neogene late-stage orogenic Pb...
Understanding the tectonic evolution of orogenic belts and intracratonic areas depends on our abilit...
The Tatric crystalline unit of the Western Carpathians in northern Slovakia displays an inverted met...
International audienceThe age of intraplate volcanism in northern Pannonian Basin of Carpathians is ...