. Transactions . h Bohutin, near Przibram. a, Cam-brian sandstone; b, pre-Carabrian schists; c, granite; cZ, main fault-fissure ; e e, diorite dikes. (Note : At Przibram itself the pre-Cara-brian schists constitute the hanging-wall of the main fault-fissure tothe entire depth of the mines—about 1110 meters, or 3600 feet.) Fig. 41.—Diagrammatic representation of the structure of theVerespatak ore-bodies (Volbura), showing the ore replacing thewashed-out cement of a breccia, mostly of porphyritic fragments. Fig. 42.—The same, only conglomerate instead of breccia. Fig. 43.—Vertical S. to N. secti
. Transactions . h Bohutin, near Przibram. a, Cam-brian sandstone; b, pre-Carabrian schists; c, granite; cZ, main fault-fissure ; e e, diorite dikes. (Note : At Przibram itself the pre-Cara-brian schists constitute the hanging-wall of the main fault-fissure tothe entire depth of the mines—about 1110 meters, or 3600 feet.) Fig. 41.—Diagrammatic representation of the structure of theVerespatak ore-bodies (Volbura), showing the ore replacing thewashed-out cement of a breccia, mostly of porphyritic fragments. Fig. 42.—The same, only conglomerate instead of breccia. Fig. 43.—Vertical S. to N. section through the Vulkoj mines,showing the supra-position of andesite upon the shaly a, Nepomuk adit; 6, sandstone; c, andesite; d, Corabia open-workings; e, Jeruga adit; /, Peter-Paul adit; gy Hermann adit. Fjg. 44.—Vertical E. to W. section through the gold-mines ofBotesiu and Vulkoj. A, Botesiu; B, Vulkoj; a, Nepomuk aditjb, sandstone; c, andesite; d, Corabia open-workings; j, Jeruga Fig. 40. Fig. 41 Fig. 42 wmwTmmmm \{ \yv \\ Fig. 43
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Keywords: ., bo, bookcentury1800, bookdecade1870, booksubjectmineralindustries
