Permitting

The project is fully permitted for all exploration activities and enjoys strong support from local government administrations.

 

Geology

The Chandman-Yol area lies within the Khyargas Nuur sub-terrane of the Pre-Cambrian to Early Paleozoic “Lake” Terrane. The structure of the area can be described as NW trending antiform structures expressed by mountain range tops. The geology at Chandman-Yol is dominated by numerous fault slices of Vend-Cambrian metasedimentary rocks (sandstone, siltstone, argillite, limestone) and volcaniclastic units. Intruded into the Vend-Cambrian sequence are numerous island arc type calc-alkalic intrusives dating to the Mid-Cambrian. A specific biotite granite phase is linked to mineralisation (Cu, Au, As, Mo, Ag, Sb, Zn, Pb) and shows broad zones of intense quartz-sericite-pyrite (+chalcopyrite) alteration, thought to represent a high-level near-typical Cu-Au porphyry system with distal iron-rich skarns.


Chandman Project - Local Geology_sm



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