On sources of substance of gold ore deposits and their water flows of dispersion; Bulletin of the Tomsk Polytechnic University; Vol. 309, № 4

On sources of substance of gold ore deposits and their water flows of dispersion; Bulletin of the Tomsk Polytechnic University; Vol. 309, № 4

Detalles Bibliográficos
Parent link:Bulletin of the Tomsk Polytechnic University/ Tomsk Polytechnic University (TPU).— , 2006-2007
Vol. 309, № 4.— 2006.— [P. 26-31]
Autor Principal: Shestakov B. I.
Summary:Заглавие с титульного листа
Электронная версия печатной публикации
On the basis of comparison of differences of ore enclosing rock clarkes with granite clarkes it is established, that gold ore deposits and their water flows contain only those elements for which this difference is positive. High correlation of values of these differences with abnormal contents of elements in ores and water flows of dispersion shows, that source of these elements are enclosing rocks. Presence of granitization fields in structure of all investigated deposits shows, that extraction of elements from enclosing rocks occurs as a result of their granitization. It is supposed, that transfer of elements is carried out by pore solutions, and their deposition occurs as a result of nonequilibrium state between pore and gravitational waters.
Idioma:inglés
Publicado: 2006
Series:Natural sciences
Subjects:
sources
substances
gold ore deposits
water flows of dispersion
clarkes
differences
ore enclosing rocks
granites
elements
correlations
values
ores
enclosing rocks
granitization
pore solutions
deposition
pore waters
gravitational waters
электронный ресурс
Acceso en liña:http://www.lib.tpu.ru/fulltext/v/Bulletin_TPU/2006/v309eng/i4/06.pdf
Formato: Electrónico Capítulo de libro
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=179800

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