Unique ore complexes in the north-western sector of the Pacific ore belts

Using hierarchic ore-formation analysis methods it is shown that thin sulfidization zones in several regions represent the formations, whose composition most fully reflects mineralogical types of polychronous and monochronous ore-formation series (ore complexes). All members of the particular series possess certain indices of mutual mineralogical-geochemical relationship. It is shown that the large thin fluidization zones in terrestrial and volcanic-origin rock massifs have, apparently, different nature - from hydrothermal-sedimentary to epigenetic (plutonic-fluid). These, practically non-investigated zones, are the most important ore substance sources at porphyric and vein field formation. Together with many satellite deposits, including monochroous copper-, gold-, tin-porphyric series, they form unique ore complexes or polychronous ore-formation series.

Авторы
Volkov A.V. 1 , Savva N.E. , Sidorov A.A. , Tomson I.N.
Журнал
Номер выпуска
3
Язык
Русский
Страницы
369-372
Статус
Опубликовано
Том
399
Год
2004
Организации
  • 1 Inst. Geol. Rudn. Mest., Petr., Min., RAN, Moscow, Russian Federation
Ключевые слова
Geochemistry; Gold deposits; Lithology; Sulfide minerals; Hierarchic ore-formation analysis; North-Western Pacific ore belts; Polychronous ore-formation series; Sulfidization zones; Ore deposit geology
Дата создания
19.10.2018
Дата изменения
19.10.2018
Постоянная ссылка
https://repository.rudn.ru/ru/records/article/record/3556/