|
Mineralisation types Mesothermal mineralisations Vein-hosted galena-sphalerite±chalcopyrite±rutile mineralisation outlined in black (photo right). Location: Agios Haralambos Iron skarns, i.e. siderite-magnetite-tremolite/actinolite replacing marble, with gold contents between 12 and 31 ppm, partly limonitised (photo lower right). Location: Myriophyto Pyritiferous, and presumably gold-bearing, structurally controlled silicified zones in granites (over impressive volumes) and in schists, partly limonitised (photo below). Location: Chalkidiki ![]() |
![]() ![]() |
| Next page |