Structural control of the Cenozoic porphyry Cu-Mo, epithermal and skarn deposits and prospects, Central Tethyan belt, Lesser Caucasus

Apatite (Ap) is also present (KA1, SEM-BSE image, microgranite, Serpieri); (c) pyrite and arsenopyrite formed first and were followed by chalcopyrite (Ccp), and enargite (Eng),

The gently to moderately dipping NE-, ~N-S- and ~E-W-oriented fracture networks along the steeply dipping deposit-scale faults were the most important structural control for

The South Armenian block (SAB) of the Lesser Caucasus orogenic belt is characterized by a long-lived Cenozoic magmatism and associated porphyry Cu-Mo and epithermal Au

Gold deposits were formed during two different geodynamic evolution stages of the Lesser Caucasus, starting with Mesozoic arc construction along the Eurasian margin, and followed

This review compiles geological, mineralogical, and isotopic data from the four largest Cu–Au epithermal deposits of the Late Cretaceous Panagyurishte mineral district,

Au-rich porphyry Cu-Au deposits (i.e., with Au/Cu ~80 × 10 –6 ) are associated with magmatic systems that have evolved at overall shallower crustal levels and for this reason can

Fault Zone Evolution and Development of a Structural and Hydrological Barrier: The Quartz Breccia in the Kiggavik Area (Nunavut, Canada) and Its Control on Uranium

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