Volumetric geochemical model of Chortovo Koryto gold-ore deposit (Patom range); IOP Conference Series: Earth and Environmental Science; Vol. 21: XVIII International Scientific Symposium in Honour of Academician M. A. Usov: Problems of Geology and Subsurface Development 7–11 April 2014, Tomsk, Russia
| Parent link: | IOP Conference Series: Earth and Environmental Science Vol. 21: XVIII International Scientific Symposium in Honour of Academician M. A. Usov: Problems of Geology and Subsurface Development 7–11 April 2014, Tomsk, Russia.— 2014.— [012004, 7 p.] |
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| Altri autori: | , |
| Riassunto: | Title screen Core sampling analysis from vertical exploration wells was conducted by the statistical methods. Assayable gold samples were analyzed by the atomic absorption method, while trace elements- emission-spectral semi-quantitative method. It was determined that the grade distribution of gold and trace elements within the deposit itself does not match one of the partition laws. Applied complex mode of processing of geochemical data provided the interpretation of anomaly geochemical field structure. The analysis of geochemical association distribution showed that their structure is concentric-zonal within bulk-metasomatic halo. The geochemical association distribution, in general, is related to hydrothermal minerogenesis stages in a deposit. Based on the mining-geological Datamine studio 3 program 3-D geochemical deposit model was plotted. Режим доступа: по договору с организацией-держателем ресурса |
| Lingua: | inglese |
| Pubblicazione: |
2014
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| Accesso online: | http://iopscience.iop.org/1755-1315/21/1/012004?fromSearchPage=true |
| Natura: | Elettronico Capitolo di libro |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=638209 |
| Riassunto: | Title screen Core sampling analysis from vertical exploration wells was conducted by the statistical methods. Assayable gold samples were analyzed by the atomic absorption method, while trace elements- emission-spectral semi-quantitative method. It was determined that the grade distribution of gold and trace elements within the deposit itself does not match one of the partition laws. Applied complex mode of processing of geochemical data provided the interpretation of anomaly geochemical field structure. The analysis of geochemical association distribution showed that their structure is concentric-zonal within bulk-metasomatic halo. The geochemical association distribution, in general, is related to hydrothermal minerogenesis stages in a deposit. Based on the mining-geological Datamine studio 3 program 3-D geochemical deposit model was plotted. Режим доступа: по договору с организацией-держателем ресурса |
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