Devonian-Carboniferous porphyry copper deposits formed at the intersection of a deep-seated fault with a series of steeply dipping faults.
References
- Jenchuraeva, R.J. (1997): Tectonic settings of porphyry-type mineralization and hydrothermal alteration in Paleozoic island arcs and active continental margins, Kyrghyz Range, (Tien Shan) Kyrghyzstan. Mineralium Deposita 32, 434-440.
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