Granitoid Massifs of the Krasnoleninsky Arch in Western Siberia

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Granitoid Massifs of the Krasnoleninsky Arch in Western Siberia : Composition, Structure, Age, and Formation Conditions. / Khotylev, A. O.; Mayorov, A. A.; Khudoley, A. K.; Ershova, V. B.; Kalmykov, G. A.; Khubanov, V. B.; Chervyakovskaya, M. V.

In: Geotectonics, Vol. 55, No. 2, 28.06.2021, p. 219-239.

Research output: Contribution to journal › Article › peer-review

Author

Khotylev, A. O. ; Mayorov, A. A. ; Khudoley, A. K. ; Ershova, V. B. ; Kalmykov, G. A. ; Khubanov, V. B. ; Chervyakovskaya, M. V. / Granitoid Massifs of the Krasnoleninsky Arch in Western Siberia : Composition, Structure, Age, and Formation Conditions. In: Geotectonics. 2021 ; Vol. 55, No. 2. pp. 219-239.

BibTeX

@article{1a800cdea0c44724acb0416d46b548ae,

title = "Granitoid Massifs of the Krasnoleninsky Arch in Western Siberia: Composition, Structure, Age, and Formation Conditions",

abstract = "In our research we summarized data obtained on the composition, structure, and geochemical characteristics of the granitoid plutons of the eastern part of the Krasnoleninsky arch of the East Siberian Plate and the age of rocks surrounding them. The Kamenny, Palyanovsky, North Kamenny and Vodorazdelny granite, granodiorite, and granosyenite plutons were emplaced in the interval of 297-261 Ma (Early-Late Permian) as melting products of the lower-middle crust at the postorogenic stage. The formation of granitoid massifs in the basement of the Em-Egovsky summit took place in the Late Devonian (Frasnian, Famennian). They differ greatly from the rocks of the Kamenny pluton in composition, degree of secondary alterations, and tectonization.",

keywords = "basement, boreholes, geochemical research, granitoids, isotopic analyses, Krasnoleninsky arch, Paleozoic, plutons, secondary alterations, West Siberia",

author = "Khotylev, {A. O.} and Mayorov, {A. A.} and Khudoley, {A. K.} and Ershova, {V. B.} and Kalmykov, {G. A.} and Khubanov, {V. B.} and Chervyakovskaya, {M. V.}",

note = "Publisher Copyright: {\textcopyright} 2021, Pleiades Publishing, Inc.",

year = "2021",

month = jun,

day = "28",

doi = "10.1134/S0016852121020059",

language = "English",

volume = "55",

pages = "219--239",

journal = "Geotectonics",

issn = "0016-8521",

publisher = "МАИК {"}Наука/Интерпериодика{"}",

number = "2",

}

RIS

TY - JOUR

T1 - Granitoid Massifs of the Krasnoleninsky Arch in Western Siberia

T2 - Composition, Structure, Age, and Formation Conditions

AU - Khotylev, A. O.

AU - Mayorov, A. A.

AU - Khudoley, A. K.

AU - Ershova, V. B.

AU - Kalmykov, G. A.

AU - Khubanov, V. B.

AU - Chervyakovskaya, M. V.

PY - 2021/6/28

Y1 - 2021/6/28

N2 - In our research we summarized data obtained on the composition, structure, and geochemical characteristics of the granitoid plutons of the eastern part of the Krasnoleninsky arch of the East Siberian Plate and the age of rocks surrounding them. The Kamenny, Palyanovsky, North Kamenny and Vodorazdelny granite, granodiorite, and granosyenite plutons were emplaced in the interval of 297-261 Ma (Early-Late Permian) as melting products of the lower-middle crust at the postorogenic stage. The formation of granitoid massifs in the basement of the Em-Egovsky summit took place in the Late Devonian (Frasnian, Famennian). They differ greatly from the rocks of the Kamenny pluton in composition, degree of secondary alterations, and tectonization.

AB - In our research we summarized data obtained on the composition, structure, and geochemical characteristics of the granitoid plutons of the eastern part of the Krasnoleninsky arch of the East Siberian Plate and the age of rocks surrounding them. The Kamenny, Palyanovsky, North Kamenny and Vodorazdelny granite, granodiorite, and granosyenite plutons were emplaced in the interval of 297-261 Ma (Early-Late Permian) as melting products of the lower-middle crust at the postorogenic stage. The formation of granitoid massifs in the basement of the Em-Egovsky summit took place in the Late Devonian (Frasnian, Famennian). They differ greatly from the rocks of the Kamenny pluton in composition, degree of secondary alterations, and tectonization.

KW - basement

KW - boreholes

KW - geochemical research

KW - granitoids

KW - isotopic analyses

KW - Krasnoleninsky arch

KW - Paleozoic

KW - plutons

KW - secondary alterations

KW - West Siberia

UR - http://www.scopus.com/inward/record.url?scp=85109353605&partnerID=8YFLogxK

U2 - 10.1134/S0016852121020059

DO - 10.1134/S0016852121020059

M3 - Article

AN - SCOPUS:85109353605

VL - 55

SP - 219

EP - 239

JO - Geotectonics

JF - Geotectonics

SN - 0016-8521

IS - 2

ER -

ID: 86066207