Oligocene tuffs at Domžale, the Ljubljana basin, Slovenia

Authors

  • Polona Kralj
  • Karel Grad

DOI:

https://doi.org/10.5474/geologija.2000.016

Abstract

Oligocene volcanics have not been found yet in the Ljubljana basin. At Domžale, fine-grained tuffs predominate, although coarse-grained and lapilli tuffs also occur. The main constituents are volcanic glass shards. The tuffs are rhyolitic in composition. Alteration is reflected in the development of clay minerals - calcic montmorillonite and illite.

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How to Cite

Kralj, P., & Grad, K. (2000). Oligocene tuffs at Domžale, the Ljubljana basin, Slovenia . Geologija, 43(2), 219–221. https://doi.org/10.5474/geologija.2000.016

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