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(granodiorite, contact aureole, spotted schist, pinite-cordierite, central Serbia)
qxpPinite-cordierite from spotted slate of the Brajkovac contactmetamorphic aureole (Dudovica locality, central Serbia)NADA VASKOVIĆ1, ZORAN NIKIĆ2, DANICA SREĆKOVIĆ-BATOĆANIN1,SUZANA ERIĆ1 & EMIN MEMOVIĆ3Abstract. The Paleozoic

somePinite-cordierite from spotted slate of the Brajkovac contact metamorphic aureole (Dudovica locality, central Serbia) 49Fig. 1. Geographic position of Dudovica locality in Serbia; A, Position of Paleozoic tectonic units

ofPinite-cordierite from spotted slate of the Brajkovac contact metamorphic aureole (Dudovica locality, central Serbia) 51Fig. 3. Chemical composition of pinitic mixture phases inSi vs. AlIV+AlVI (A) and Fe+Mg vs. Si (B) diagram;


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(alluvial aquifers, water supply wells, mineral incrustations, bacteria, central Serbia)
generally below 150mV (Table 2).Clogging of water supply wells in alluvial aquifers by mineral incrustations, central Serbia 75Fig. 2. Simplified hydrogeological cross section from tube well Bnz-1 to Bn-6Table 1. General data for

(1992) concluded that theClogging of water supply wells in alluvial aquifers by mineral incrustations, central Serbia 77Fig. 4. Box-plot of low-crystallinity Mn(OH)2 proportionsof incrustations in different geochemical e

the entire source decreasedClogging of water supply wells in alluvial aquifers by mineral incrustations, central Serbia 79Fig. 7. XRD pattern of incrustation from well RB-3m (Belgrade groundwater source). Legend: Sd, siderite