UNIVERSITY EDUCATION IN MINING AT THE BEGINNING OF THE THIRD MILLENIUM
Journal Title: UNKNOWN - Year 2001, Vol 13, Issue 1
Abstract
A short review of the world mining situation at the begining of the new millenium is given. A comparison betveen the mining industries of Croatia and the USA regarding production per capi ta is presented. The basic information about the European Mining Coures (EMC) is also given, as wetl as about the university education in mining at the Faculty of Mining, Geology and Petroleum Fngineering in Zagreb.
Authors and Affiliations
Slavko Vujec
Keywords
Related Articles
- EP ID EP29920
- DOI -
- Views 182
- Downloads 2
ASHES AS AN AGENT FOR CEMENT-LIME BASED SOLIDIFICATION/STABILIZATION OF THE HAZARDOUS WASTE
One of the common treatment methods for the hazardous waste is the cement and cement-lime based solidification/stabilization (S/S). This article deals with the possibility of currently used recipe modification using flui...
Svjetlosno onečišćenje grada Zagreba u periodu prosinac 2010. - srpanj 2011
Svjetlosno onečišćenje povećanje je prirodne vrijednosti osvjetljenja okoliša kao posljedica ljudskog djelovanja. U uvodu članka dajemo pregled uzroka i posljedica svjetlosnog onečišćenja te opisujemo tri osnovne metode...
Utjecaj Tektonskog Sklopa na Formiranje Površinskog Kopa u Kamenolomu Dolomita Zaprešički Ivanec kraj Zagreba
U kamenolomu dolomita »Zaprešički Ivanec« kraj Zagreba odvija se eksploatacija u sklada s podacima dobivenim analizom tektonskog sklopa, određivanja brzina uzdužnih valova metodom refrekcijske seizmike i mjerenjima seizm...
CHEMICAL AND GEOCHEMICAL CHARACTERISTICS OF THE ČEMERNICA ANTIMONITE DEPOSIT IN THE MID-BOSNIAN SCHIST MOUNTAINS
The Čemernica Sb-Zn-Hg-W quartz vein system is situated in Lower Palaeozoic metasediments formed under 3-5 kbars and 350° to 450 °C, intruded by Upper Palaeozoic rhyolites. K-Ar dating indicated three metamorphic phases....
WEATHERING PROCESS IN EOCENE FLYSCH IN REGION OF SPLIT (CROATIA)
The Eocene flysh in the region of Split (Dalmatia, Croatia) is char¬acterized by the presence of layers with different characteristics. It mainly includes thin-layered marls, clayey marls, calcareous marls, clastic lay¬e...