master's thesis
Seizmostratigrafske značajke pleistocenskih naslaga u srednjem dijelu Jadranskog podmorja
diplomski rad
Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. urn:nbn:hr:169:595866

Gotšlih, Branimir
University of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
Department of Geology and Geological Engineering

Cite this document

Gotšlih, B. (2018). Seizmostratigrafske značajke pleistocenskih naslaga u srednjem dijelu Jadranskog podmorja : diplomski rad (Master's thesis). Retrieved from https://urn.nsk.hr/urn:nbn:hr:169:595866

Gotšlih, Branimir. "Seizmostratigrafske značajke pleistocenskih naslaga u srednjem dijelu Jadranskog podmorja : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. https://urn.nsk.hr/urn:nbn:hr:169:595866

Gotšlih, Branimir. "Seizmostratigrafske značajke pleistocenskih naslaga u srednjem dijelu Jadranskog podmorja : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. https://urn.nsk.hr/urn:nbn:hr:169:595866

Gotšlih, B. (2018). 'Seizmostratigrafske značajke pleistocenskih naslaga u srednjem dijelu Jadranskog podmorja : diplomski rad', Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, accessed 04 August 2021, https://urn.nsk.hr/urn:nbn:hr:169:595866

Gotšlih B. Seizmostratigrafske značajke pleistocenskih naslaga u srednjem dijelu Jadranskog podmorja : diplomski rad [Master's thesis]. Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering; 2018 [cited 2021 August 04] Available at: https://urn.nsk.hr/urn:nbn:hr:169:595866

B. Gotšlih, "Seizmostratigrafske značajke pleistocenskih naslaga u srednjem dijelu Jadranskog podmorja : diplomski rad", Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb, 2018. Available at: https://urn.nsk.hr/urn:nbn:hr:169:595866

Islandora Bookmark - Please login to use this feature