Mantle magma-thermofluidodynamic and intracrustal granitoid-hydrothermal-metasomatic auriferous systems; Bulletin of the Tomsk Polytechnic University; Vol. 311, № 1
| Parent link: | Bulletin of the Tomsk Polytechnic University/ Tomsk Polytechnic University (TPU).— , 2006-2007 Vol. 311, № 1.— 2007.— [P. 34-42] |
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| Hovedforfatter: | |
| Summary: | Заглавие с титульного листа Электронная версия печатной публикации Contents of typical models of formation of abyssal and intra-core ore-forming systems are discussed. As it has been already marked, the interaction between core and mantle ore-forming systems occurred at formation of large and unique golden-ore deposits. The interaction of the abyssal mantle substance with formations of the Earth's crust has been carried out by penetration of high-temperature gas-fluids, magmatic melts and solid bodies, forming diapiric magma-thermofluidodynamic systems on borders of the inner core with the bottom mantle and within the limits of the upper mantle - the Earth's crust |
| Sprog: | engelsk |
| Udgivet: |
2007
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| Serier: | Geology and minerals |
| Fag: | |
| Online adgang: | http://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2007/v311eng/i1/06.pdf |
| Format: | Electronisk Book Chapter |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=182495 |
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| 200 | 1 | |a Mantle magma-thermofluidodynamic and intracrustal granitoid-hydrothermal-metasomatic auriferous systems |b Electronic resource |f A. F. Korobeynikov | |
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| 225 | 1 | |a Geology and minerals | |
| 230 | |a Электронные текстовые данные (1 файл :878 Кб) | ||
| 300 | |a Заглавие с титульного листа | ||
| 300 | |a Электронная версия печатной публикации | ||
| 320 | |a [Bibliography: p. 42 (30 titles)] | ||
| 330 | |a Contents of typical models of formation of abyssal and intra-core ore-forming systems are discussed. As it has been already marked, the interaction between core and mantle ore-forming systems occurred at formation of large and unique golden-ore deposits. The interaction of the abyssal mantle substance with formations of the Earth's crust has been carried out by penetration of high-temperature gas-fluids, magmatic melts and solid bodies, forming diapiric magma-thermofluidodynamic systems on borders of the inner core with the bottom mantle and within the limits of the upper mantle - the Earth's crust | ||
| 337 | |a Adobe Reader | ||
| 461 | 1 | |0 (RuTPU)RU\TPU\book\169973 |t Bulletin of the Tomsk Polytechnic University |f Tomsk Polytechnic University (TPU) |d 2006-2007 | |
| 463 | 1 | |0 (RuTPU)RU\TPU\book\197808 |x 1684-8519 |t Vol. 311, № 1 |v [P. 34-42] |d 2007 |p 139 p. | |
| 610 | 1 | |a mantle magma-thermofluidodynamic auriferous systems | |
| 610 | 1 | |a granitoid-hydrothermal-metasomatic auriferous systems | |
| 610 | 1 | |a auriferous systems | |
| 610 | 1 | |a ore-forming systems | |
| 610 | 1 | |a golden-ore deposits | |
| 610 | 1 | |a Earth's crust | |
| 610 | 1 | |a gas-fluids | |
| 610 | 1 | |a magmatic melts | |
| 610 | 1 | |a solid bodies | |
| 610 | 1 | |a mantle | |
| 610 | 1 | |a труды учёных ТПУ | |
| 610 | 1 | |a электронный ресурс | |
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| 700 | 1 | |a Korobeynikov |b A. F. | |
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