Petrological characterization of montsogranites and granosigenites of the Ubukunskoye ore occurrence
About authors
- 1 — Russian State Geological Prospecting University
- 2 — Russian State Geological Prospecting University
Abstract
Granites with monzonitic structure and granosienites represent early and late phases of intrusion development. Crystallization of granites takes place with deanortitization of plagioclase and incongruent formation of К-Na-feldspar. Granosienites are characterized with cotectic crystallization. Changes in granosienites at the acid stage lead to albitization of the K-Na-feldspar, chloritization of biotite and large-scale development of pyrite with Cu, Cd, Zn, Pb impurities. The late alkaline stage is characterized with sedimentation of Ca as calci-spar.
Similar articles
Filtering hydrocyclone for drilling mud cleaning with filter sounding by running transverse ultrasonic waves
2008 L. V. Vukadinovich
Development of the traction electric drive of the trolley transportation for the open-cast mining works
2008 V. A. Cherepanov
Investigations of character of manifestation of mountain pressure in various mining-geological conditions
2008 A. V. Rogachkov