Only if tectonic processes provide a pathway from a source rock to a hostrock and along with these tectonic processes a physical-chemical regime change takes place favorable for the concentration of the commodity in question
mineral ores can indeed be found in various tectonic environments, certain types of ores are more commonly associated with specific tectonic settings. For example:
Divergent Boundaries: These areas often host basaltic magmatism and can be rich in copper, zinc, and lead.
Convergent Boundaries: These regions, especially subduction zones, are known for porphyry copper deposits and gold.
Transform Boundaries: These areas might not be as rich in mineral deposits compared to the other two, but they can still host gold and silver.