RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES3004, doi:10.2205/2017ES000603, 2017


Figure 2. Depth section of Muruntau deposit along line Mine M – SG-10 well. 1 – metasandstone, silty sandstone; 2 – aleurolite, aleuropelite; 3 – albite-quartz schist; 4 – crystalline and carbonaceous-albite-quartz schist; 5 – siliceous and quartz rocks; 6 – quartz-feldsparic-micaceous pegmatites; 7 – granosyenite, quartz-porphyry and etc.; 8 – granite leucocratic; 9 – "dome fold" of biotititated (porphyroblast) quartz-two-feldspar contact-metasomatic rocks; 10 –zone of scarn (actinolite-clinozoisite and diopside-garnet-actinolitic assemblages); 11 – zone of massive linear-vein and lens shaped quartz-feldspar mineralization; 12 – Au-metalliferous deposits and stoops; 13 – ore bodies eroded and supposititous; 14 – aggregate ore transport faults; 15 – ore-hosting and blocking faults; 16 – minings: a) mine-M, b) boreholes. Enclosing rocks: R$_{2-3}$ts – crystalline and carbonaceous-albite-quartz schist with assise of quartz and siliceous-carbonate rocks. G$_3$-O$_2$bs$_2$ – metasandstone metaaleurolite of puckered and schistic structure, micaceous-albite-quartz schist with adit levels and lense of chalcedony. G$_3$-O$_2$bs$_2$ – aleurolite-microschist with assises of carbon-micaceous-quartz schists with adit levels and lense of siliceous rocks and carbonates.


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Citation: Ezhkov Yu. B., R. R. Rakhimov, R. R. Rustamjonov, I. V. Novikova (2017), Ore-geochemical zonality and gold complex potential of Muruntau, Russ. J. Earth Sci., 17, ES3004, doi:10.2205/2017ES000603.


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