Mineralogical and Chemical Characteristics of Marble of Bela Pola deposite
Abstract
This paper presents mineralogical characteristics of marbles from the Bela Pola deposit. We have made mineralogical-chemical analyses of marbles and associated minerals in them. The investigation was carried out at the Faculty of natural and technical sciences – Štip. Marbles from Bela Pola are dolomite and dolomite-calcite types. Microscope investigations have shown that marbles from Bela Pola have granoblastic structure but at some places it can be found with porphyroblastic structures. Percentage on calcite and dolomite is: 94.08% dolomite, 6.25% is calcite in white marbles. On the other hand calcite is present with 93% in gray marbles. Except dolomite and calcite also appear the following accessoring minerals: quartz, fluorite, corundum and paragonite. In general, after summarizing all the facts, which have resulted from this research we could say that, the Bela Pola marbles are massive, compact and white with high quality. In accordance to all formerly mentioned features, this marbles can be classified in the commercial group of marbles suitable for external application or internal design.Downloads
References
Dufour, M., Koltsov, A., Zolotarev, A., Kuznetsov, A., 2007: Corundum – bearing metasomatic rocks in the Central Pamirs, Petrology, 15, 2, 151–167.
Klein, C., and Hurlbut, C. S., 1993: Manual of Mineralogy (after J. D. Dana), 21st edition. John Wiley & Sons, Inc., New Jork, 681 p.
Марић Л., 1940: Петрографска и геолошка грађа околине Прилепа и СИ од Прилепа, Весник Геол. Инст. Краљ. Југ. кн. VII – Београд.
Okrusch, M., Bunch, T. E., Bank, H., 1976: Paragenesis and petrogenesis of a corundum – bearing marble at Hunza (Kashmir) Mineralium Deposita, Volume 11, Issue 3, pp 278–297.
Robbins, M., 1994: Fluorescence: Gems and Minerals under Ultraviolet Light: Geosciences Press, Inc., Phoenix, Arizona, 374 p.
Стојанов Р., 1958: Преtходни резулtаtи од gеолошките и pеtроgрафските истражувања на Селечка планина, Трудови на Геолошкиот завод на НРМ, св. 6, Скопје.
Стојанов Р., 1960: Претходни резултати од геолошките и pеtрографските истражувања на високометаморфните стени во централниот дел на Пелаgонискиот масив, Трудови на Геолошкиот завод на НРМ, св. 7, Скопје.