2017
DOI: 10.1134/s1075701517060034
|View full text |Cite
|
Sign up to set email alerts
|

Tectono-Magmatic Cycles and Geodynamic Settings of Ore-Bearing System Formation in the Southern Cis-Argun Region

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

0
3
0

Year Published

2018
2018
2023
2023

Publication Types

Select...
7

Relationship

1
6

Authors

Journals

citations
Cited by 11 publications
(3 citation statements)
references
References 41 publications
0
3
0
Order By: Relevance
“…The spatial distribution of favorable ore mineralization regions with intensity from 0.6 to 1 agrees well with the productivity of oregenesis stages, which have passed in the interval from the Proterozoic to the Holocene inclusive. The most productive minerogenic event occurred in the Mesozoic era when during the process of intraplate tectonomagmatic activation the subalcalic magmatics were formed with Au, Cu-Mo-, Pb-Zn-Ag-metallogenic specialization, volcano-plutonic calder complexes with Mo-U, Pb-Zn, and fluorite ores, and then rare-metal granites with a Sn-W-Li-Ta mineralization spectrum [31]. In connection with the manifestation of Mesozoic magmatism, there were also processes of hydrothermal-metasomatic alterations in rocks from magnesian and calcareous skarns, K-feldspars, greisens and beresites to hydromicas and argillizites took place [30].…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…The spatial distribution of favorable ore mineralization regions with intensity from 0.6 to 1 agrees well with the productivity of oregenesis stages, which have passed in the interval from the Proterozoic to the Holocene inclusive. The most productive minerogenic event occurred in the Mesozoic era when during the process of intraplate tectonomagmatic activation the subalcalic magmatics were formed with Au, Cu-Mo-, Pb-Zn-Ag-metallogenic specialization, volcano-plutonic calder complexes with Mo-U, Pb-Zn, and fluorite ores, and then rare-metal granites with a Sn-W-Li-Ta mineralization spectrum [31]. In connection with the manifestation of Mesozoic magmatism, there were also processes of hydrothermal-metasomatic alterations in rocks from magnesian and calcareous skarns, K-feldspars, greisens and beresites to hydromicas and argillizites took place [30].…”
Section: Discussionmentioning
confidence: 99%
“…Geological structure and ore-bearing volcano-plutonic complexes of the southern Argun area evolved during the Proterozoic (which ended about 600 million years ago), Caledonian (520-410 million years ago), and Hercynian tectonomagmatic cycles (360-120 million years ago), in the process of tectonomagmatic activation in the late Mesozoic (160-100 million years ago) and at the neotectonic phase of the region's development. Late Mesozoic tectonomagmatic activation is most productive in the form of ore-genetic processes that determined the metallogenic appearance of the territory [30,31].…”
Section: Geological Settingmentioning
confidence: 99%
“…[Bortnikov and Petrov, 2020]. Most of the ore deposits are associated with the Late Mesozoic tectonomagmatic activation, which was the most productive in the manifestation of tectonotermal events and ore-genetic processes that determine metallogenic territory's image [Andreeva et al, 2020;Petrov et al, 2017a]. However, the territory is not provided with a system of continuous observations after lithosphere deformation, although further prospects of MRB development are linked here with work on deep horizons of longterm exploitable deposits under complicated geological and mining conditions.…”
Section: Improvement Of Methods For Forecasting and Preventing Technogenic Accidentsmentioning
confidence: 99%