MINERALOGY OF THE OVERBURDEN ROCKS OF THE KOKLAN W-MO DEPOSIT (SOUTH URALS)
The Koklan W-Mo deposit is overlapped by Mesozoic-Cenozoic rocks 120–140 m thick, which may be subdivided in four members on the basis of variable proportions of the rock-forming minerals (quartz, hydromica (with glauconite), smectites and X-ray amorphous phase) and the presence of clinoptilolite an...
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| Language: | English |
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South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
2015-06-01
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| Series: | Минералогия |
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| Online Access: | https://journal.mineralogy.ru/wp-content/uploads/2019/09/2015-2-8.pdf |
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| author | E.V. Belogub K.А. Novoselov E.E. Palenova P.V. Khvorov |
| author_facet | E.V. Belogub K.А. Novoselov E.E. Palenova P.V. Khvorov |
| author_sort | E.V. Belogub |
| collection | DOAJ |
| description | The Koklan W-Mo deposit is overlapped by Mesozoic-Cenozoic rocks 120–140 m thick, which may be subdivided in four members on the basis of variable proportions of the rock-forming minerals (quartz, hydromica (with glauconite), smectites and X-ray amorphous phase) and the presence of clinoptilolite and calcite. Mineral composition was identified using an X-ray diffractometry. The horizon of oolitic iron ores occurs at the bottom of sedimentary sequence. The consistent composition of members throuth the section indicates stable formation conditions of sedimentary sequence and promising use of overburden rocks during exploitation of the deposit. |
| format | Article |
| id | doaj-art-104b428dc6a947c8a678b768a7a38eaa |
| institution | DOAJ |
| issn | 2313-545X 2782-2044 |
| language | English |
| publishDate | 2015-06-01 |
| publisher | South Urals Federal Research Center of Mineralogy and Geoecology UB RAS |
| record_format | Article |
| series | Минералогия |
| spelling | doaj-art-104b428dc6a947c8a678b768a7a38eaa2025-08-20T02:57:48ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442015-06-01127784MINERALOGY OF THE OVERBURDEN ROCKS OF THE KOKLAN W-MO DEPOSIT (SOUTH URALS)E.V. Belogub0K.А. Novoselov1 E.E. Palenova2P.V. Khvorov3Institute of Mineralogy UB RASInstitute of Mineralogy UB RASInstitute of Mineralogy UB RASInstitute of Mineralogy UB RASThe Koklan W-Mo deposit is overlapped by Mesozoic-Cenozoic rocks 120–140 m thick, which may be subdivided in four members on the basis of variable proportions of the rock-forming minerals (quartz, hydromica (with glauconite), smectites and X-ray amorphous phase) and the presence of clinoptilolite and calcite. Mineral composition was identified using an X-ray diffractometry. The horizon of oolitic iron ores occurs at the bottom of sedimentary sequence. The consistent composition of members throuth the section indicates stable formation conditions of sedimentary sequence and promising use of overburden rocks during exploitation of the deposit.https://journal.mineralogy.ru/wp-content/uploads/2019/09/2015-2-8.pdfglauconiteclinoptilolitecomprehensive utilization of resources |
| spellingShingle | E.V. Belogub K.А. Novoselov E.E. Palenova P.V. Khvorov MINERALOGY OF THE OVERBURDEN ROCKS OF THE KOKLAN W-MO DEPOSIT (SOUTH URALS) Минералогия glauconite clinoptilolite comprehensive utilization of resources |
| title | MINERALOGY OF THE OVERBURDEN ROCKS OF THE KOKLAN W-MO DEPOSIT (SOUTH URALS) |
| title_full | MINERALOGY OF THE OVERBURDEN ROCKS OF THE KOKLAN W-MO DEPOSIT (SOUTH URALS) |
| title_fullStr | MINERALOGY OF THE OVERBURDEN ROCKS OF THE KOKLAN W-MO DEPOSIT (SOUTH URALS) |
| title_full_unstemmed | MINERALOGY OF THE OVERBURDEN ROCKS OF THE KOKLAN W-MO DEPOSIT (SOUTH URALS) |
| title_short | MINERALOGY OF THE OVERBURDEN ROCKS OF THE KOKLAN W-MO DEPOSIT (SOUTH URALS) |
| title_sort | mineralogy of the overburden rocks of the koklan w mo deposit south urals |
| topic | glauconite clinoptilolite comprehensive utilization of resources |
| url | https://journal.mineralogy.ru/wp-content/uploads/2019/09/2015-2-8.pdf |
| work_keys_str_mv | AT evbelogub mineralogyoftheoverburdenrocksofthekoklanwmodepositsouthurals AT kanovoselov mineralogyoftheoverburdenrocksofthekoklanwmodepositsouthurals AT eepalenova mineralogyoftheoverburdenrocksofthekoklanwmodepositsouthurals AT pvkhvorov mineralogyoftheoverburdenrocksofthekoklanwmodepositsouthurals |