Whole-rock geochemistry and U-Pb ages of Devonian bimodal-type rhyolites from the Rudny Altai, Russia: Petrogenesis and tectonic settings

Kuibida, M. L.; Murzin, O. V.; Крук, Н. Н.; Safonova, Inna; Sun, Min; Komiya, Tsuyoshi; Wong, J.; Aoki, Shogo; Murzina, N.M.; Николаева, И. В.; Семенова, Д. В.; Khlestov, M. V.; Shelepaev, R.A.; Котлер, П. Д.; Yakovlev, V.A.; Naryzhnova, A. V.

doi:10.1016/j.gr.2019.12.002

Cited by 11 publications

(8 citation statements)

References 120 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…Therefore, the study area was covered by a marginal sea of this ocean. This is confirmed by the studies of Cocks and Torsvik [11], Domeier [19], Kuibida et al [12], and Wilhem et al [14], who also explained the highly complex regime of interactions of blocks now constituting the Altai. The Rudny Altai was located in tropical latitudes (approximately 30 °N) during the De- The Altai belongs to the Central Asian Orogenic Belt-a gigantic chain of orogens stretching across Eurasia [9,10].…”

Section: Geological Settingmentioning

confidence: 57%

“…The Altai consist of a series of elongated terranes (slices) accreted to the periphery of the former continent of Siberia (now a part of the Eurasian lithospheric plate), and one of these terranes is the Rudny Altai [11][12][13][14]. This domain of the Russian Altai is dominated by Paleozoic complexes (sedimentary, volcanic, plutonic, and metamorphic), from which the Devonian volcano-sedimentary sequences with a total thickness of up to 5000 m are the most widespread on the study area, i.e., near Zmeinogorsk [12]. These rocks were formed in a marine basin on an active periphery of the Siberian continent where the above-mentioned terranes interacted with the formation of island arcs and back-arc basins.…”

Section: Geological Settingmentioning

confidence: 99%

“…The Rudny Altai was located in tropical latitudes (approximately 30 °N) during the De- The Altai belongs to the Central Asian Orogenic Belt-a gigantic chain of orogens stretching across Eurasia [9,10]. The Altai consist of a series of elongated terranes (slices) accreted to the periphery of the former continent of Siberia (now a part of the Eurasian lithospheric plate), and one of these terranes is the Rudny Altai [11][12][13][14]. This domain of the Russian Altai is dominated by Paleozoic complexes (sedimentary, volcanic, plutonic, and metamorphic), from which the Devonian volcano-sedimentary sequences with a total thickness of up to 5000 m are the most widespread on the study area, i.e., near Zmeinogorsk [12].…”

Section: Geological Settingmentioning

confidence: 99%

See 2 more Smart Citations

New Marine Geoheritage from the Russian Altai

Gutak

Ruban

Yashalova

2021

JMSE

View full text Add to dashboard Cite

Marine geoheritage comprises unique geological features of modern and ancient seas and oceans. The Russian Altai (southern Siberia) is a vast and geologically rich area, which was covered by a marginal sea of the Panthalassa Ocean in the Devonian. New geosites representing shallow- and deep-marine depositional environments and palaeoecosystems of submarine volcano slopes are proposed, namely, Melnichnye Sopki and Zavodskie Sopki. They are located near the town of Zmeinogorsk (Altai Region of the Russian Federation). These pieces of marine geoheritage are valuable on an international scale. Special geoconservation procedures are recommended to manage the proposed geosites efficiently. They can be included in a geopark, which is reasonable to create due to the concentration of geological and mining heritage in the study area.

show abstract

Section: Geological Settingmentioning

confidence: 57%

Section: Geological Settingmentioning

confidence: 99%

Section: Geological Settingmentioning

confidence: 99%

See 1 more Smart Citation

New Marine Geoheritage from the Russian Altai

Gutak

Ruban

Yashalova

2021

JMSE

View full text Add to dashboard Cite

show abstract

“…(1) Middle Late Paleozoic Rudny-Altai zone that formed on the Siberian active margin as a result of the subduction of Ob-Zaisan oceanic plate [9][10][11];…”

Section: Geological Structures and Metallogenic Zones Of The Great Altaimentioning

confidence: 99%

“…and complex compositions of rich ores, with high concentrations of Cu + Pb + Zn and impurities. 6), and Artemiev (7) deposits in Irtysh (Ir) district; Zolotukhino (8) and Orlovka (9) deposits in Zolotushino (Zo) district; Zmeinogorsk (10) and Korbalikha (11) deposits in Zmeinogorsk (Zm) district; Talaya (12) and Rubtsovsk (13) deposits in Rubtsovsk (Ru) district. 6), and Artemiev (7) deposits in Irtysh (Ir) district; Zolotukhino (8) and Orlovka (9) deposits in Zolotushino (Zo) district; Zmeinogorsk (10) and Korbalikha (11) deposits in Zmeinogorsk (Zm) district; Talaya (12) and Rubtsovsk (13) deposits in Rubtsovsk (Ru) district.…”

Section: Rudny-altai Metallogenic Beltmentioning

confidence: 99%

Geological History of the Great Altai: Implications for Mineral Exploration

et al. 2022

View full text Add to dashboard Cite

The Great Altai region, located at the boundary of Russia, Mongolia, China, and Kazakhstan, belongs to the system of the Central Asian Orogenic Belt. It has undergone a long complex geological and metallogenic history. Extremely rich resources of base, precious, and rare metals (Fe, Cu, Pb, Zn, Ag, Au, Li, Cs, Ta, Nb, REE, etc.) maintain developed mining and metallurgical industry, especially in East Kazakhstan, which is the key metallogenic province. The East Kazakhstan province comprises the Rudny Altai, Kalba-Narym, West-Kalba, and Zharma-Saur metallogenic belts, each having its typical mineralization profiles and deposits. The reconstructed geodynamic and metallogenic history of the Great Altai province, along with the revealed relationships between tectonic settings and mineralization patterns, allowed us to formulate a number of geodynamic, structural, lithostratigraphic, magmatic, mineralogical, and geochemical criteria for exploration and appraisal of mineral potential in Eastern Kazakhstan. Geodynamic criteria are based on the origin of different mineralization types in certain geodynamic settings during the Late Paleozoic–Early Mesozoic orogenic cycle. Structural criteria mean that the location of base-metal deposits in Rudny Altai, gold deposits in the West Kalba belt, rare and base metals in the Kalba-Narym and Zharma-Saur zones is controlled by faults of different sizes. Lithostratigraphic criteria consist of the relation of orebodies with certain types of sedimentary or volcanic-sedimentary rocks. Magmatic criteria are due to the relation between mineralization types and igneous lithologies. Mineralogical and geochemical criteria include typical minerals and elements that can serve as tracers of mineralization. The joint use of all these criteria will open new avenues in prospecting and exploration at a more advanced level.

show abstract