GREEN DIOPSIDE WITH MAUVE TERMINATION FROM THE BAZHENOVSKOE CHRYSOTILE-ASBESTOS DEPOSIT, CENTRAL URALS
Some generations of diopside from rodingite (skarn?) veins of the Bazhenovskoe chrysotileasbestos deposit have complex crystallization evolution with the formation of zonal-sectorial polychrome crystals. The paper considers one example of diopside, the color of which is caused by Mn/Fe ratio in diff...
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South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
2021-06-01
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| Series: | Минералогия |
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| Online Access: | https://journal.mineralogy.ru/wp-content/uploads/2021/07/2021_7_2_4.pdf |
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| author | V.A. Popov |
| author_facet | V.A. Popov |
| author_sort | V.A. Popov |
| collection | DOAJ |
| description | Some generations of diopside from rodingite (skarn?) veins of the Bazhenovskoe chrysotileasbestos deposit have complex crystallization evolution with the formation of zonal-sectorial polychrome crystals. The paper considers one example of diopside, the color of which is caused by Mn/Fe ratio in different elements of crystal anatomy. For example, the green color is typical of growth pyramids of faces {100}, {010}, {001}, {310}, whereas mauve color is observed in those of {831} and {22 1 }. The anatomy elements of red color exhibit maximum Mn contents. |
| format | Article |
| id | doaj-art-7f829978a2034c6799d4833de471ab2a |
| institution | Kabale University |
| issn | 2313-545X 2782-2044 |
| language | English |
| publishDate | 2021-06-01 |
| publisher | South Urals Federal Research Center of Mineralogy and Geoecology UB RAS |
| record_format | Article |
| series | Минералогия |
| spelling | doaj-art-7f829978a2034c6799d4833de471ab2a2025-02-12T08:45:18ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442021-06-0172788110.35597/2313-545X-2021-7-2-4GREEN DIOPSIDE WITH MAUVE TERMINATION FROM THE BAZHENOVSKOE CHRYSOTILE-ASBESTOS DEPOSIT, CENTRAL URALSV.A. Popov0South Urals Federal Research Center of Mineralogy and Geoecology UB RASSome generations of diopside from rodingite (skarn?) veins of the Bazhenovskoe chrysotileasbestos deposit have complex crystallization evolution with the formation of zonal-sectorial polychrome crystals. The paper considers one example of diopside, the color of which is caused by Mn/Fe ratio in different elements of crystal anatomy. For example, the green color is typical of growth pyramids of faces {100}, {010}, {001}, {310}, whereas mauve color is observed in those of {831} and {22 1 }. The anatomy elements of red color exhibit maximum Mn contents.https://journal.mineralogy.ru/wp-content/uploads/2021/07/2021_7_2_4.pdfdiopsidecrystal shape and anatomyparageneses |
| spellingShingle | V.A. Popov GREEN DIOPSIDE WITH MAUVE TERMINATION FROM THE BAZHENOVSKOE CHRYSOTILE-ASBESTOS DEPOSIT, CENTRAL URALS Минералогия diopside crystal shape and anatomy parageneses |
| title | GREEN DIOPSIDE WITH MAUVE TERMINATION FROM THE BAZHENOVSKOE CHRYSOTILE-ASBESTOS DEPOSIT, CENTRAL URALS |
| title_full | GREEN DIOPSIDE WITH MAUVE TERMINATION FROM THE BAZHENOVSKOE CHRYSOTILE-ASBESTOS DEPOSIT, CENTRAL URALS |
| title_fullStr | GREEN DIOPSIDE WITH MAUVE TERMINATION FROM THE BAZHENOVSKOE CHRYSOTILE-ASBESTOS DEPOSIT, CENTRAL URALS |
| title_full_unstemmed | GREEN DIOPSIDE WITH MAUVE TERMINATION FROM THE BAZHENOVSKOE CHRYSOTILE-ASBESTOS DEPOSIT, CENTRAL URALS |
| title_short | GREEN DIOPSIDE WITH MAUVE TERMINATION FROM THE BAZHENOVSKOE CHRYSOTILE-ASBESTOS DEPOSIT, CENTRAL URALS |
| title_sort | green diopside with mauve termination from the bazhenovskoe chrysotile asbestos deposit central urals |
| topic | diopside crystal shape and anatomy parageneses |
| url | https://journal.mineralogy.ru/wp-content/uploads/2021/07/2021_7_2_4.pdf |
| work_keys_str_mv | AT vapopov greendiopsidewithmauveterminationfromthebazhenovskoechrysotileasbestosdepositcentralurals |