Archaeological findings of malachite ore pieces, and objects made of malachite or copper, raise the question of where the raw material was mined. Research in this direction is a challenge in modern applied mineralogy, especially concerning minerals from the oxidation zone of copper-bearing ores. According to recent studies in this field, a complex research method, including impurity elements, will provide a better distinction between different sources. The present paper is focused on the content of impurity elements in malachite ore samples from copper deposits in the Rosen ore field, SE Bulgaria, with mining activity in the past: Propadnala Voda, Sarneshko Kladenche, Meden Rid, Korucheshme, and Rosen. The nickel concentration obtained by LA-ICP-MS analyses is above 1000 ppm (1012.80–1505.15 ppm) in all studied samples, accompanied by the following element impurities: Zn, Co, Mg, As, Sb, Fe, Ag, Au, Sn, Se, and Te. The quantitative concentrations of Zn, Co, Mg, As, Ag, and Se vary in different ranges in the examined malachites from each locality. Based on this, it seems possible to differentiate between samples of each mineralization. These data would have to be supplemented by the analyses of more malachite ore samples from the region.
In 1939, one of the first summarizing works of the famous Bulgarian geologist Georgi Bonchev “Contribution to the springs in Bulgaria” related to groundwater in the country was published. In his field research, the author visited and described about 60 natural springs or groups of springs with temperatures from 20 °C to over 75 °C, attached to different tectonic zones, over 40 lukewarm and cold springs with mineralized waters and about 290 karst and other cold springs. This article is also relevant for modern hydrogeology. The presented general picture of the locations of the springs, the discharge and qualities of the waters from the natural springs before 1939 allows making comparisons of the occurred changes due to natural and anthropogenic factors.
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