Academy of Sciences of the Czech Republic, v
Based on geochemical, isotopic and age similarities with the Panafrican (ultra)mafic layered intrusive complexes in Hoggar and the geological background, we prefer the Cadomian age of intrusions, and (4) apatite fission-track analysis of gabbroic samples from Korolupy and Maříž and the Číměř granite indicate very similar ages of 150.2 ... ................
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