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master's thesis
Mineraloške, geokemijske i mikromorfološke karakteristike krednog paleotla u kamenolomu Tri jezerca
diplomski rad

Horvat, Viktor
University of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
Department of Mineralogy, Petrology and Mineral Resources

Cite this document

Horvat, V. (2014). Mineraloške, geokemijske i mikromorfološke karakteristike krednog paleotla u kamenolomu Tri jezerca : diplomski rad (Master's thesis). Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering. Retrieved from https://urn.nsk.hr/urn:nbn:hr:169:804782

Horvat, Viktor. "Mineraloške, geokemijske i mikromorfološke karakteristike krednog paleotla u kamenolomu Tri jezerca : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2014. https://urn.nsk.hr/urn:nbn:hr:169:804782

Horvat, Viktor. "Mineraloške, geokemijske i mikromorfološke karakteristike krednog paleotla u kamenolomu Tri jezerca : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2014. https://urn.nsk.hr/urn:nbn:hr:169:804782

Horvat, V. (2014). 'Mineraloške, geokemijske i mikromorfološke karakteristike krednog paleotla u kamenolomu Tri jezerca : diplomski rad', Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, accessed 04 October 2024, https://urn.nsk.hr/urn:nbn:hr:169:804782

Horvat V. Mineraloške, geokemijske i mikromorfološke karakteristike krednog paleotla u kamenolomu Tri jezerca : diplomski rad [Master's thesis]. Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering; 2014 [cited 2024 October 04] Available at: https://urn.nsk.hr/urn:nbn:hr:169:804782

V. Horvat, "Mineraloške, geokemijske i mikromorfološke karakteristike krednog paleotla u kamenolomu Tri jezerca : diplomski rad", Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb, 2014. Available at: https://urn.nsk.hr/urn:nbn:hr:169:804782

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