ACCESSORY SULFIDES OF THE KEMPIRSAI ULTRAMAFIC MASSIF, SOUTHERN URAL

DOI: 10.24411/0869-5997-2018-10013

Authors

  • Yurichev А.N.
    Tomsk State University
    nt

Keywords:

Southern Ural, Kempirsai massif, ultramafites, accessory sulphides, chemistry, genesis.

Abstract

Studies were performed for accessory sulfides from dunites and massive chromitites occurring at AlmazZhemchuzhina chromite deposit of the Kempirsai ultramafic massif which is the largest massif of restitic ultramafites in the Southern Ural. Three genetic groups of sulphides associated with various processes of their host ultramafic rocks formation and transformation have been identified. Typomorphic and chemical features of sulfides are characterized.

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Published

2020-12-10

How to Cite

Юричев Алексей Николаевич. (2020). ACCESSORY SULFIDES OF THE KEMPIRSAI ULTRAMAFIC MASSIF, SOUTHERN URAL: DOI: 10.24411/0869-5997-2018-10013. Ores and Metals, (4). Retrieved from https://rm.tsnigri.ru/index.php/main/article/view/113

Issue

No. 4 (2018)

Section

Geology of ore deposits