Mantle magma-thermofluidodynamic and intracrustal granitoid-hydrothermal-metasomatic auriferous systems

Mantle magma-thermofluidodynamic and intracrustal granitoid-hydrothermal-metasomatic auriferous systems

Detalles Bibliográficos
Parent link:Bulletin of the Tomsk Polytechnic University/ Tomsk Polytechnic University (TPU).— , 2006-2007
Vol. 311, № 1.— 2007.— [P. 34-42]
Autor Principal: Korobeynikov A. F.
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
Idioma:inglés
Publicado: 2007
Series:Geology and minerals
Subjects:
mantle magma-thermofluidodynamic auriferous systems
granitoid-hydrothermal-metasomatic auriferous systems
auriferous systems
ore-forming systems
golden-ore deposits
Earth's crust
gas-fluids
magmatic melts
solid bodies
mantle
труды учёных ТПУ
электронный ресурс
Acceso en liña:http://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2007/v311eng/i1/06.pdf
Formato: Electrónico Capítulo de libro
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=182495

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