Diagenesis to very low-grade metamorphism in Lower Palaeozoic sediments: a case study from deep borehole Tobolka 1, the Barrandian Basin, Czech Republic

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Authors

SUCHÝ Václav SANDLER Amir SLOBODNÍK Marek SÝKOROVÁ Ivana FILIP Jiří MELKA Karel ZEMAN Antonín

Year of publication 2015
Type Article in Periodical
Magazine / Source International Journal of Coal Geology
MU Faculty or unit

Faculty of Science

Citation
Doi http://dx.doi.org/10.1016/j.coal.2014.12.015
Field Geology and mineralogy
Keywords Graptolite; Chitinozoan; Illite-smectite; Fluid inclusion; Apatite; Petroleum
Description Research deal with the diagenetic grade of a 2.7 km thick sequence of lower Palaeozoic marine sediments in the Tobolka 1 deep exploration borehole and these was investigated by analysing organic and mineral components and fluid inclusions embedded in vein minerals. The combined evidence from organic matter, clay minerals and fluid inclusions points to maximum paleotemperatures of ~ 100–230 °C in the Silurian–Devonian strata, and up to ~ 250 °C or even higher in the Ordovician strata. Apatite fission track analysis (AFTA) data suggests that maximum heating occurred between 340 and 380 Ma, i.e. during Variscan orogenic deformations. These paleotemperatures and the degree of diagenesis may have been produced by a post-Middle Devonian burial or tectonic load that was subsequently eroded, or by higher paleogeothermal gradients, or by a combination of both.
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