Old Au-bearing arsenopyrite deposit.
Skarn-like mineralization due to metasomatism in the exocontact zone of the Variscan Klodzko-Zloty Stok granodiorite massif.
Note on the mineral list:
Mikulski (1996) also mentions Ni-Fe-Co sulpharsenides.
References:
- S. Z. Mikulski (1996): Gold mineralization within contact-metamorphic and shear zones in the `Zloty Jar' quarry - the Zloty Stok As-Au deposit area (Sudetes). Kwartalnik Geologiczny, 40(3), 407–442.
| Group 1 - Elements | | Gold | 1.AA.05 | | | Group 2 - Sulphides and Sulfosalts | | Arsenopyrite | 2.EB.20 | | | Löllingite | 2.EB.15a | | | Pyrrhotite | 2.CC.10 | | Fe | | S | | , (-4M), also given as Fe | | S (x = 0 - 0.2) |
| | Group 4 - Oxides and Hydroxides | | Quartz | 4.DA.05 | | | Group 5 - Nitrates and Carbonates | | Calcite | 5.AB.05 | | | Group 7 - Sulphates, Chromates, Molybdates and Tungstates | | Hydroniumjarosite | 7.BC.10 | | | Scheelite | 7.GA.05 | | | Group 9 - Silicates | | Chrysotile (TL) | 9.ED.15 | | | Unclassified Minerals | | Clinochrysotile | - | | | 'Garnet Group' | - | | X | | Z | | (TO | | ) | | (X = Ca, Fe, etc·, Z = Al, Cr, etc·, T = Si, As, V) |
| | 'Pyroxene Group' | - | |
|
12 entries listed. 9 valid minerals.
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