Jiří Žák

TL;DR: In this article, the authors summarized the current knowledge on the nature, kinematics and timing of movement along major tectonic boundaries in the Bohemian Massif and demonstrates how the Variscan plutonism and deformation evolved in space and time.

TL;DR: The Central Bohemian Plutonic Complex (CBPC) consists of episodically emplaced plutons, the internal fabrics of which recorded tectonic evolution of a continental magmatic arc as mentioned in this paper.

TL;DR: In this article, it was shown that the internal contacts along the eastern margin of the Tuolumne batholith are highly variable; the contacts range from relatively sharp, to gradational boundaries, to sheeted zones, to very complex boundaries formed by multiple processes.

TL;DR: The Tuolumne Intrusive Complex, an upper-crustal (7-11 km emplacement depths), incrementally constructed plutonic complex (~1100 km 2 ), preserves evidence from several data sets indicating the repeated, multiscale, magmatic erosion of older units occurred and that some eroded material was recycled into younger magma batches.

TL;DR: The Sazava pluton (∼354 Ma) of the Central Bohemian Plutonic Complex was emplaced syntectonically into the upper crustal Neo-Proterozoic and Lower Paleozoic host rock along the SE margin of the Tepla-Barrandian Zone, Bohemian Massif (Czech Republic).