Mineralisierungszonen
Mineralisierungszonen, often referred to as zones of mineralization or ore zones, represent areas within the Earth's crust where economically significant concentrations of metallic or non-metallic minerals have accumulated. These zones are the direct result of geological processes that concentrate elements from dispersed sources into localized, high-grade deposits. The formation of mineralisierungszonen is typically a complex interplay of tectonic activity, magmatic intrusions, hydrothermal fluid circulation, and weathering.
Hydrothermal processes are a primary driver in the creation of many mineralisierungszonen. Superheated fluids, often derived
The economic viability of a mineralisierungszone is determined by the concentration and accessibility of the valuable