M.Sc. Tezi Görüntüleme | |||||||||||||||||||||
|
|
||||||||||||||||||||
Summary:
Ore minerals in wall rocks occur as a result of replacement and void fillings. They are are mainly sphalerite, galena, chalcopyrite; lesser pyrite, Ag-bearing fahlerz and native gold. Void fillings in the vein consist of quartz, zeolite and calcite. The structure of the ore is a breccia filling type. Ore minerals in breccia are also fractured by later tectonic activites and silisify. These fractures are mailnly filled by silica.
|