1.

Volcanic facies analysis of a subaqueous basalt lava-flow complex at Hruškovec, NW Croatia - evidence of advanced rifting in the Tethyan domain

The Hruškovec quarry is situated within the Zagorje–Mid-Transdanubian zone. The Triassic volcanic-sedimentary sequence is incorporated into the Jurassic–Cretaceous mélange. Discovery of peperite within Triassic rocks, with registration of conodonts, links its origin to magmatism during rifting in a progressively subsiding basin during the Triassic. It precludes an affiliation of the subaqueous basaltic lava flow with the ophiolite formation. The basaltic rocks may be correlated with advanced Triassic rifting, and related volcanic-sedimentary successions along the Tethyan orogenic belt.

F.02 Acquisition of new scientific knowledge

COBISS.SI-ID: 1580885

2.

Application of paleontological and stratigraphical methods in modern science

The presentation is focused to application of paleontological and stratigraphical methods in modern science.

B.03 Paper at an international scientific conference

COBISS.SI-ID: 1679445

3.

Hindeodus-Isarcicella population in the lowermost Triassic of western Slovenia

Documentation of the first conodont fauna of the Hindeodus-Isarcicella group in the Permian-Triassic interval of western Slovenia.

B.03 Paper at an international scientific conference

COBISS.SI-ID: 1464661

4.

First record of conodont fauna in the Permian-Triassic boundary interval of NW Serbia

Results of conodont study of the Komirić section in Serbia are presented. This is first documentation of the Late Permian conodonts in the Dinarides.

B.03 Paper at an international scientific conference

COBISS.SI-ID: 1464917