МОНГОЛЫН ЦАЙР-ХАРТУГАЛГАНЫ ОРДУУДЫН АНГИЛАЛ
Abstract
The classification of lead-zinc deposits and ore occurrences in Mongolia is mainly based on mineral association, rocks which are genetically related to Pb, Zn mineralization, host litology, ore structure, and alteration.
The deposits and occurrences of lead-zinc mineralization in Mongolia in the report are classified into five ore formation: polymetal calcic skarn related to subalkaline granite, granosyenite, mezothermal lead-zinc related to subalkaline polyphase intrusions, mesothermal cupper-lead-zinc related to subaerial extrusive rocks, epithermal silver-lead related to felsic extrusive rocks and telethermal leaf fine formation in carbonate rocks. All ore formation of lead-zinc deposits can be subdhided into several models. The leader role belongs to tire Fe-Zn (Cd, In) skarn md mezothermal Zn-Pb-Ag (Au) models.
Downloads
References
Батжаргал.Ш. Доржготов.Д. О главнейщих-формационных типах полиметаплинеского оруденения Монголии. /Тезисы докладов научно-нрактическоп конференции по свинду и цинку МНР/ 1985,с.11-15
Гарамжав.Д, Зарянов.Ю П, Доржготов.Д. Рудные формации и минеральные тппы месторождений их прогнозная оценка. В кн: Геология и полезные ископаемые МНР. М., Недра, 1989, с.126-134 .
З.Яковлев.В.А. Медь, свинец и цинк. В кн: Геология МНР. М., Недра, 1977, с.141-146.
Dennis P.COX and Donald A.Singer. Mineral Deposit Models, U.S.Geol. Survey bulletin 1963.P.1-10
Dorjgotov D. Distribution map of polymetallic deposits and occurrences in Mongolia. Scale 1:3000000. 1998
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2023 Геологийн асуудлууд
This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.
