ИИ

И. И. Лиханов

V.S. Sobolev Institute of Geology and Mineralogy

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ВВ

В. В. Ревердатто

V.S. Sobolev Institute of Geology and Mineralogy

ПС

П. С. Козлов

V.S. Sobolev Institute of Geology and Mineralogy

A. D. Nozhkin

V.S. Sobolev Institute of Geology and Mineralogy

O. P. Polyansky

V.S. Sobolev Institute of Geology and Mineralogy

S. V. Zinoviev

V.S. Sobolev Institute of Geology and Mineralogy

КА

К. А. Савко

Voronezh State University

НВ

Н. В. Попов

Russian Scientific Research Institute Microbe

ВВ

В. В. Хиллер

Zavaritsky Institute of Geology and Geochemistry

ОМ

О. М. Turkina

V.S. Sobolev Institute of Geology and Mineralogy

АА

А. А. Krylov

All Russian Research Institute of Geology and Mineral Resources of the World Ocean

Cooperative Institutions

Russian Academy of Sciences

V.S. Sobolev Institute of Geology and Mineralogy

Novosibirsk State University

Siberian Branch of the Russian Academy of Sciences

Czech Academy of Sciences, Institute of Geology

Institute of Mineralogy

Siberian Research Institute of Geology, Geophysics and Mineral Resources

Zavaritsky Institute of Geology and Geochemistry

Institute of the Earth’s Crust

Institute of Petroleum Geology and Geophysics

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Three metamorphic events in the precambrian P-T-t history of the Transangarian Yenisey ridge recorded in garnet grains in metapelites

Petrology (2013)

И. И. Лиханов В. В. Ревердатто П. С. Козлов В. В. Хиллер В. П. Сухоруков

Riphean

Orogeny

Geochronology

10.1134/s0869591113060040

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Citations (33)

Zoning of garnets as an indicator of metamorphic evolution in metapelites of the Yenisei Ridge

Doklady Earth Sciences (2014)

И. И. Лиханов В. В. Ревердатто

Grossular

Anorthite

Anorthosite

10.1134/s1028334x14090098

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Citations (7)

Sapphirine-bearing granulites of the anabar shield

Геохимия (2019)

A. D. Nozhkin И. И. Лиханов К. А. Савко А. А. Krylov Pavel Serov

The results of a detailed study of the mineral and chemical composition, geothermobarometry, and U-Pb isotope dating of zircon of high-aluminous sapphirine-bearing crystals of shales associated with biotite-garnet-sillimanite gneisses, hypersthene-two feldspar and high-potassium hypersthene orthogneisses, Ti-rich and subalkaline metabasites belonging to the Kilegirian Formation of the Daldyn series of the Anabar shield. Unlike the known granulites of the Daldin and Upper Ananbar series, the rocks of this association are enriched in K, Rb, Ba, Th, light REEs, differing in elevated (La/Yb)n. The results of thermobarometry yielded the P–Tparameters of formation and evolution of sapphirine-bearing granulites in the Anabar shield with peak values of UHT metamorphism in the range of T= 920–1000°C at P= 9–11 kbar. Isotope-geochronological data indicate a polymetamorphic evolution of these rocks. Detrital zircon cores in the center of crystals yielded ages of 3.36, 2.75, 2.6, and 2.5 Ga. Later, superimposed metamorphic transformations of the detrital zircon formed rims dated to 2.4, 2.3, 2.2, and 1.8 Ga. The timing of formation of aluminous metasedimentary and associated metamagmatic rocks can be estimated in the interval from 2.5 to 2.4 billion years. A potential provenance source of the detrital zircons could be hypersthene plagiogneisses and metabasites of the Daldyn series with a premetamorphic age no less than 3.3 Ga, and products of their metamorphism of about 2.7 Ga old, and possibly not yet detected in the region Na-K granites with an age of about 2.6–2.5 billion years, known on other shields and enriched with radioactive (K, Th, U) and rare elements. An additional source of clastic material in the formation of aluminous sediments could be the associated two feldspar magmatic rocks of rhyolite composition, having the same model age with them.

Baltic Shield

10.31857/s0016-7525645486-502

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Citations (0)

Mineral assemblages of the Al2SiO5 “triple point” in metapelites

Doklady Earth Sciences (2013)

И. И. Лиханов В. В. Ревердатто

Triple point

10.1134/s1028334x13010121

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Citations (6)

Mineral Geothermobarometry

Springer geology (2018)

В. В. Ревердатто И. И. Лиханов O. P. Polyansky V. S. Sheplev V Yu Kolobov

Geothermobarometry

TRACE (psycholinguistics)

10.1007/978-3-030-03029-2_2

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Citations (4)

Contact metamorphism of Fe- and Al-rich graphitic metapelites in the Transangarian region of the Yenisei Ridge, eastern Siberia, Russia

Lithos (2001)

И. И. Лиханов В. В. Ревердатто V. S. Sheplev A.E. Verschinin П. С. Козлов

Andalusite

Geothermobarometry

Cordierite

Sillimanite

Muscovite

Staurolite

Isograd

10.1016/s0024-4937(01)00048-2

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Citations (68)

Provenance of Precambrian Fe‐ and Al‐rich Metapelites in the Yenisey Ridge and Kuznetsk Alatau, Siberia: Geochemical Signatures

Acta Geologica Sinica - English Edition (2007)

И. И. Лиханов В. В. Ревердатто

Abstract: Major, trace and rare earth element contents of Fe‐ and Al‐rich metapelites from the Korda (Yenisey Ridge) and Amar (Kuznetsk Alatau) formations were determined to examine the nature, origin and evolution of their protoliths. Results indicate that these rocks are the redeposited and metamorphosed products of Precambrian kaolinitic weathering crusts, while the geochemical distinctions between the studied metapelites are determined by different weathering conditions in the source area and tectonic settings. The protolith of the Korda Formation metapelites was produced by erosion products of the post‐Archean granitoid rocks, which accumulated under humid climate conditions in shallow‐water basins along the continental margin. The geochemical characteristics of the deeper primary deposits of the Amar Formation suggest that volcanogenic material of mafic composition derived from an island‐arc environment had a major role in supplying the erosion zone. These results agree with lithofacies data and with the geodynamic reconstruction of the evolution of the Yenisey Ridge and Kuznetsk Alatau during the Mesoproterozoic and Neoproterozoic, respectively. It was shown that REEs had limited mobility during contact metamorphism. The coherent mobility of REEs during collisional metamorphism may be attributed both to mineral reactions responsible for modal changes and to local chemical heterogeneity inherited from the initial protolith.

Protolith

Baltica

10.1111/j.1755-6724.2007.tb00964.x

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Citations (35)

Age of blastomilonites of the Yenisei regional shear zone as evidence of the Vendian accretionary-collision events at the western margin of the Siberian Craton

Doklady Earth Sciences (2013)

И. И. Лиханов В. В. Ревердатто С. В. Зиновьев A. D. Nozhkin

Continental Margin

Rodinia

Collision zone

Accretionary wedge