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Václav Kachlík

Researcher at Charles University in Prague

Publications -  44
Citations -  1015

Václav Kachlík is an academic researcher from Charles University in Prague. The author has contributed to research in topics: Massif & Geology. The author has an hindex of 19, co-authored 34 publications receiving 849 citations.

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A plate-kinematic model for the assembly of the Bohemian Massif constrained by structural relationships around granitoid plutons

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.
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New evidence of blueschist facies rocks and their geotectonic implication for Variscan suture(s) in the Bohemian Massif

TL;DR: In this paper, the presence of the Variscan suture, which straddles the SE margin of Saxothuringian Zone from Erzgebirge to Sudetes, and its possible continuation to the Moldanubian Zone, was identified.
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The 40Ar/39Ar ages from the West Sudetes (NE Bohemian Massif): constraints on the Variscan polyphase tectonothermal development

TL;DR: In this article, the West Sudetes (NE margin of the Bohemian Massif) consist of a complex mosaic of several tectonometamorphic units juxtaposed during the Variscan orogeny.
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Multistage magma emplacement and progressive strain accumulation in the shallow‐level Krkonoše‐Jizera plutonic complex, Bohemian Massif

TL;DR: In this article, field relationships combined with new U-Pb zircon geochronology suggest that the shallow-level Krkonose-Jizera plutonic complex, northern Bohemian Massif, was assembled successively from bottom to top, starting with emplacement of the separately evolved S-type Tanvald granite (317.3 ± 2.1 Ma), followed by at least two voluminous batches of the I-type porphyritic Liberec (319.5
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Transition from island-arc to passive setting on the continental margin of Gondwana: U–Pb zircon dating of Neoproterozoic metaconglomerates from the SE margin of the Teplá–Barrandian Unit, Bohemian Massif

TL;DR: In this paper, the authors used SHRIMP and LA ICP-MS U-Pb ages of pebbles of granitic rocks and detrital zircons from Neoproterozoic Vletice metaconglomerates of the SE margin of the Tepla-Barrandian Unit were used to characterize the regional geotectonic setting at the Protean/Paleozoic boundary.