undergraduate thesis
Petrografske karakteristike granatnog granita S-tipa kamenoloma Puklice, sjeverozapadni Papuk
završni rad

Vilenica, Leonarda
University of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
Department of Mineralogy, Petrology and Mineral Resources

Cite this document

Vilenica, L. (2020). Petrografske karakteristike granatnog granita S-tipa kamenoloma Puklice, sjeverozapadni Papuk : završni rad (Undergraduate thesis). Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering. Retrieved from https://urn.nsk.hr/urn:nbn:hr:169:066543

Vilenica, Leonarda. "Petrografske karakteristike granatnog granita S-tipa kamenoloma Puklice, sjeverozapadni Papuk : završni rad." Undergraduate thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2020. https://urn.nsk.hr/urn:nbn:hr:169:066543

Vilenica, Leonarda. "Petrografske karakteristike granatnog granita S-tipa kamenoloma Puklice, sjeverozapadni Papuk : završni rad." Undergraduate thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2020. https://urn.nsk.hr/urn:nbn:hr:169:066543

Vilenica, L. (2020). 'Petrografske karakteristike granatnog granita S-tipa kamenoloma Puklice, sjeverozapadni Papuk : završni rad', Undergraduate thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, accessed 09 October 2024, https://urn.nsk.hr/urn:nbn:hr:169:066543

Vilenica L. Petrografske karakteristike granatnog granita S-tipa kamenoloma Puklice, sjeverozapadni Papuk : završni rad [Undergraduate thesis]. Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering; 2020 [cited 2024 October 09] Available at: https://urn.nsk.hr/urn:nbn:hr:169:066543

L. Vilenica, "Petrografske karakteristike granatnog granita S-tipa kamenoloma Puklice, sjeverozapadni Papuk : završni rad", Undergraduate thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb, 2020. Available at: https://urn.nsk.hr/urn:nbn:hr:169:066543

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