Palaeozoic and Mesozoic Geological Development in Bosnia and Herzegovina
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The Geological Foundation of Bosnia and Herzegovina
Sediments were fractured and collected. The deposition of Silurian sediments, which subsequently serve as the basis for all other geological strata and the relief of Bosnia and Herzegovina, ceased more than 400 million years ago. Upon this Silurian base, layers from the early and late Palaeozoic era (i.e., the Devonian and Carboniferous periods) were deposited in the same ocean basin.
Palaeozoic Sediments: Composition and Distribution
The Palaeozoic sediments are presented mostly as clastic and less commonly as carbonate formations, which are metamorphosed in some places. Palaeozoic sediments can mainly be found in the following regions:
- The Una-Sana area
- The Central Bosnian Schist Mountains
- Eastern