4.1 Article

HOW MANY EXTENSIONAL STAGES MARKED THE VARISCAN GRAVITATIONAL COLLAPSE IN THE BOHEMIAN MASSIF?

Journal

ANNALES SOCIETATIS GEOLOGORUM POLONIAE
Volume 91, Issue 2, Pages 121-136

Publisher

POLISH GEOLOGICAL SOC
DOI: 10.14241/asgp.2021.08

Keywords

Gravitational collapse; anisotropy of magnetic susceptibility; U-Pb zircon geochronology; Variscan orogen; Central Bohemian plutonic complex

Categories

Funding

  1. Czech Science Foundation (GACR) [19-02177Y]
  2. Institute of Geology, Czech Academy of Sciences [RVO: 67985831]

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The tectonic development of the Variscan belt in Central Europe involved both compression and extensional phases related to gravitational collapse, resulting in the formation of sedimentary basins and magmatic bodies. The Benesov pluton, for example, exhibited primary magmatic fabrics and deformational fabrics indicating extensional stages. The study revealed a three-stage extensional history during the gravitational collapse, highlighting the complex succession of individual extensional stages rather than a simple process.
Tectonic development of the Variscan belt in Central Europe included, besides important compression, also an extensional phase related to gravitational collapse, which governed the origin of many sedimentary basins and magmatic bodies. One of these bodies is the Benesov pluton, featuring primary magmatic fabrics as well as deformational fabrics, related to subsequent extensional stages. Recognition of these fabrics and their links to other significant extension-induced structures in the Bohemicum and Moldanubicum not only sheds new light on the pluton itself but also extends a general knowledge of deformational stages, accompanying gravitational collapse of the Variscan orogen. The authors found that this pluton was strongly strained in a normal-faulting regime under brittle-ductile conditions. The age of deformation is constrained by a magmatic age of 347 +/- 3 Ma and by the age of Carboniferous sedimentary cover. New data indicate a three-stage extensional history during the phase of gravitational collapse: (1) Tournaisian extension (similar to 350-345 Ma) within arc-related tonalitic intrusions; (2) late Visean to Serpukhovian extension (similar to 332-320 Ma), connected to the brittle-ductile unroofing and origin of a NE-SW basin system; and (3) Gzhelian to Cisuralian extension (similar to 303-280 Ma), related to normal faulting and sedimentation in Permo-Carboniferous troughs, elongated NNE-SSW. Consequently, the gravitational collapse studied involved a complex succession of individual extensional stages, rather than a simple process.

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