Accessory Minerals of the Galmoenan Mafic-Ultramafic Massif, Koryak Upland, Kamchatka


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Abstract

A group of accessory ore minerals is revealed in rocks of the Galmoenan mafic-ultramafic massif (Koryak Upland, Kamchatka, Russia), represented by native metals (iron, copper, zinc, and silver), iron-nickel and cobalt-iron intermetallic compounds, sulfides (pentlandite, cobaltpentlandite, pyrrhotite, sphalerite, heazlewoodite, millerite, shandite, pyrite, chalcopyrite, and Cu3S2 phase), arsenides (maucherite, nicolite, orcelite, and modderite), and some other minerals. Their chemical compositions, crystal forms, and paragenetic associations are described. Formation of these minerals is attributed to serpentinization of rocks.

About the authors

E. G. Sidorov

Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Sciences

Author for correspondence.
Email: mineral@kscnet.ru
Russian Federation, Petropavlovsk-Kamchatsky, 683006

E. I. Sandimirova

Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Sciences

Email: mineral@kscnet.ru
Russian Federation, Petropavlovsk-Kamchatsky, 683006

V. M. Chubarov

Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Sciences

Email: mineral@kscnet.ru
Russian Federation, Petropavlovsk-Kamchatsky, 683006

V. V. Anan’ev

Institute of Volcanology and Seismology, Far East Branch of the Russian Academy of Sciences

Email: mineral@kscnet.ru
Russian Federation, Petropavlovsk-Kamchatsky, 683006

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