Natural electric fields in Siberian gold deposits: structure, origin, and relationship with gold orebodies; Russian Geology and Geophysics; Vol. 58, iss. 8

Bibliografiset tiedot
Parent link:Russian Geology and Geophysics: Scientific Journal
Vol. 58, iss. 8.— 2017.— [P. 984-989]
Päätekijä: Erofeev L. Ya. Leonid Yakovlevich
Yhteisötekijät: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геофизики (ГЕОФ), Национальный исследовательский Томский политехнический университет (ТПУ) Физико-технический институт (ФТИ) Кафедра общей физики (ОФ)
Muut tekijät: Orekhov A. N. Aleksandr Nikolaevich, Erofeeva G. V. Galina Vasiljevna
Yhteenveto:Title screen
Characteristics of the constant natural electric field in the Siberian gold ore areas are given. The regularities of spatial variations in the electric-field potential and the parameters and properties of anomalies have been established. The cause of the natural electric field in deposits of major genotypes has been elucidated. It is shown that the electric field is induced mainly by physicochemical processes running in electron-conducting syn-ore metasomatites and by circulation of groundwaters. Orebodies do not influence significantly the structure of the observed electric fields. We give recommendations on application of the electric-field method at various gold ore objects.
Режим доступа: по договору с организацией-держателем ресурса
Kieli:englanti
Julkaistu: 2017
Aiheet:
Linkit:https://doi.org/10.1016/j.rgg.2017.07.009
Aineistotyyppi: Elektroninen Kirjan osa
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=655685
Kuvaus
Yhteenveto:Title screen
Characteristics of the constant natural electric field in the Siberian gold ore areas are given. The regularities of spatial variations in the electric-field potential and the parameters and properties of anomalies have been established. The cause of the natural electric field in deposits of major genotypes has been elucidated. It is shown that the electric field is induced mainly by physicochemical processes running in electron-conducting syn-ore metasomatites and by circulation of groundwaters. Orebodies do not influence significantly the structure of the observed electric fields. We give recommendations on application of the electric-field method at various gold ore objects.
Режим доступа: по договору с организацией-держателем ресурса
DOI:10.1016/j.rgg.2017.07.009