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Geology and mineralogy of ore at the hidden Engteri Au-Ag deposit, the Magadan Region

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Abstract

The Engteri is a new hidden Au-Ag deposit in the Russian segment of the Pacific ore belt. The discovery of this deposit merits special attention, because it involves repeated attempts to reappraise a lowprospective ore occurrence, which were crowned with success as a result of fulfillment of large-scale drilling project. The average Au grade is 18.6 gpt. The deposit is classified as the gold geochemical type of Au-Ag deposits. The major ore mineral is pyrite, which amounts to no less than 95% of the total ore minerals. The native phases comprise electrum and to a lesser extent native gold of low fineness (730). The homogenization temperature of fluid inclusions is 125–255°C with a distinct maximum at 145–150°C. Despite blind localization of some orebodies, the Engteri deposits bears evidence for a deep erosion level: (1) small vertical range of economic mineralization (50–100 m); (2) predominant occurrence of massive sugarlike quartz with a low sulfide content; (3) prevalence of massive and brecciated textures above rhythmically banded textures; and (4) lack of low-temperature propylites. The southern part of the ore field distinguished by occurrence of rhythmically banded, framework-tabular, and brecciated texture has the best prospect for revealing new orebodies. The Engteri deposit allowed us to outline the following prospecting guides and methods of prospecting for hidden Au-Ag deposits: (1) these deposits are regularly arranged in ore clusters between heavy concentrate anomalies of cinnabar and gold-silver or silver-base-metal occurrences (method of missed link); (2) findings of fragments of ore mineral assemblages with sporadically high Au and Ag contents in barren calcite-quartz veins (method of indicators); (3) linear zones of ankeritization in the fields of low- and mediumtemperature propylites (mapping of metasomatic rocks); and (4) pyrite-quartz veinlets with rhythmically banded pockets (mineralogical mapping of halos of stringer-disseminated mineralization).

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Correspondence to A. V. Obushkov.

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Original Russian Text © A.V. Obushkov, S.F. Struzhkov, M.V. Natalenko, O.B. Ryzhov, S.G. Kryazhev, Yu.I. Radchenko, 2010, published in Geologiya Rudnykh Mestorozhdenii, 2010, Vol. 52, No. 6, pp. 512–533.

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Obushkov, A.V., Struzhkov, S.F., Natalenko, M.V. et al. Geology and mineralogy of ore at the hidden Engteri Au-Ag deposit, the Magadan Region. Geol. Ore Deposits 52, 459–478 (2010). https://doi.org/10.1134/S1075701510060036

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