(Figure 1).Water 2021, 13, 3269 Water 2021, 13, x FOR PEER Critique Water 2021, 13, x FOR PEER
(Figure 1).Water 2021, 13, 3269 Water 2021, 13, x FOR PEER Evaluation Water 2021, 13, x FOR PEER REVIEW10 of 16 11 of 17 11 ofFigure Concentration distribution map of of Sb, reporting areas of sampling points (with Figure 7.7. Concentration distribution mapSb, reporting Safranin supplier places of sampling points (with indicaFigure 7. Concentration distribution map of Sb, reporting places of sampling points (with indication of these exceeding the MACs) and main mineral deposits; AZD4625 supplier tectonic lineaments (white tion of those exceeding the connected associated MACs) and key mineral deposits; tectonic lineaments indication of are also illustrated. related MACs) and main mineral deposits; tectonic lineaments (white lines) these exceeding the lines) are also illustrated. (white lines) are also illustrated.Figure eight. Concentration distribution map of Cr, reporting locations of sampling points (with Figure eight. Concentration distribution map of Cr,and key mineral deposits; tectonic lineaments Figure eight. Concentration distribution map of Cr, reporting areas of sampling points (with indicaindication of those exceeding the associated MACs) reporting places of sampling points (with indication of are also illustrated. MACs) and major mineral deposits; tectonic lineaments (white tion of these exceeding the related related MACs) and principal mineral deposits; tectonic lineaments (white lines) these exceeding the (white lines) are also illustrated. lines) are also illustrated.Punctual geogenic sources are associated to the occurrences of metalliferous ores within the Ionian side on the Peloritani Mts, consisting of Fe-Pb-Zn-Cu-Sb-As-Ag mineralization, accompanied by quartz, fluorite, barite and siderite [31]. Anthropogenic sources are linked towards the heavy urbanized coastal locations, each on the Tyrrhenian and Ionian sides, and to the industrial and electric energy plants in the Barcellona ilazzo Plain [11]. A comparable behavior is shown by Ni distribution (Figure ten), with reduce concentrations characterizing the inner sectors in the mountain chain, and maxima with points exceeding the connected MAC mostly situated within the easternmost part of the studied region and linked to mineral deposits. Precisely the same is for Cu (Figure 11) distribution, with higher concentrations within the coastal regions and reduced concentrations in the inner zones. The maximum concentrations are discovered once again close towards the mineralization on the Ionian side.Water 2021, 13, 3269 Water 2021, 13, x FOR PEER Assessment Water 2021, 13, x FOR PEER REVIEW11 of 16 12 of 17 12 ofFigure 9. Concentration distribution map of Pb, reporting areas of sampling points (with Figure 9. Concentration distribution map of Pb, reporting places of sampling points (with indicaFigure 9. Concentration distribution map of Pb, reporting areas of sampling points (with indication of these exceeding the MACs) and key mineral deposits; tectonic lineaments (white tion of these exceeding the connected related MACs) and principal mineral deposits; tectonic lineaments indication of are also illustrated. connected MACs) and most important mineral deposits; tectonic lineaments (white lines) these exceeding the lines) are also illustrated. (white lines) are also illustrated.Figure 10. Concentration distribution map of Ni, reporting places of sampling points (with Figure 10. Concentration distribution map of Ni, reporting areas of sampling points (with of Ni, reporting locations of sampling points (with Figure ten. of these exceeding the related MACs) and primary mineral deposits;.
