Middle Paleozoic Rhyolite of the Gorny and Rudny Altai

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Middle Paleozoic Rhyolite of the Gorny and Rudny Altai : Geochronology and Composition. / Kuibida, M. L.; Timkin, V. I.; Krivchikov, V. A. et al.

In: Doklady Earth Sciences, Vol. 487, No. 2, 01.08.2019, p. 885-889.

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

Harvard

Kuibida, ML, Timkin, VI, Krivchikov, VA, Murzin, OV, Krupchatnikov, VI, Popova, OM, Kruk, NN, Rudnev, SN, Kuibida, YV, Shokal’sky, SP, Gusev, NI, Komiya, T, Aoki, S, Sun, M & Naryzhnova, AV 2019, 'Middle Paleozoic Rhyolite of the Gorny and Rudny Altai: Geochronology and Composition', Doklady Earth Sciences, vol. 487, no. 2, pp. 885-889. https://doi.org/10.1134/S1028334X19080130

APA

Kuibida, M. L., Timkin, V. I., Krivchikov, V. A., Murzin, O. V., Krupchatnikov, V. I., Popova, O. M., Kruk, N. N., Rudnev, S. N., Kuibida, Y. V., Shokal’sky, S. P., Gusev, N. I., Komiya, T., Aoki, S., Sun, M., & Naryzhnova, A. V. (2019). Middle Paleozoic Rhyolite of the Gorny and Rudny Altai: Geochronology and Composition. Doklady Earth Sciences, 487(2), 885-889. https://doi.org/10.1134/S1028334X19080130

Vancouver

Kuibida ML, Timkin VI, Krivchikov VA, Murzin OV, Krupchatnikov VI, Popova OM et al. Middle Paleozoic Rhyolite of the Gorny and Rudny Altai: Geochronology and Composition. Doklady Earth Sciences. 2019 Aug 1;487(2):885-889. doi: 10.1134/S1028334X19080130

Author

Kuibida, M. L. ; Timkin, V. I. ; Krivchikov, V. A. et al. / Middle Paleozoic Rhyolite of the Gorny and Rudny Altai : Geochronology and Composition. In: Doklady Earth Sciences. 2019 ; Vol. 487, No. 2. pp. 885-889.

BibTeX

@article{2a7a35c36f424c4cb90a249f7b38337f,

title = "Middle Paleozoic Rhyolite of the Gorny and Rudny Altai: Geochronology and Composition",

abstract = "Abstract: The paper reports the results of geological, geochemical, and isotope–geochronological studies of subvolcanic rhyolites of NW Gorny Altai and Rudny Altai, which belong to the large Hercynian volcanic systems: Altai-Minusa and Altai–Salair, respectively. U–Pb zircon dating revealed two age groups: ~410–405 and 390–381 Ma. The isotope–geochemical characteristics of the rhyolites demonstrate high εNd(Т) from +2.6 to 6.0 with relatively young model ages T(DM) = 851–966 Ma in Rudny Altai and older model ages, up to 1266 Ma, in NW Gorny Altai. The rhyolites show transitional geochemical signatures between within-plate and island-arc felsic magmas. The results obtained are consistent with two-stage evolution of volcanism and its migration from the continent to the ocean.",

keywords = "AGE",

author = "Kuibida, {M. L.} and Timkin, {V. I.} and Krivchikov, {V. A.} and Murzin, {O. V.} and Krupchatnikov, {V. I.} and Popova, {O. M.} and Kruk, {N. N.} and Rudnev, {S. N.} and Kuibida, {Y. V.} and Shokal{\textquoteright}sky, {S. P.} and Gusev, {N. I.} and T. Komiya and S. Aoki and M. Sun and Naryzhnova, {A. V.}",

note = "Publisher Copyright: {\textcopyright} 2019, Pleiades Publishing, Ltd.",

year = "2019",

month = aug,

day = "1",

doi = "10.1134/S1028334X19080130",

language = "English",

volume = "487",

pages = "885--889",

journal = "Doklady Earth Sciences",

issn = "1028-334X",

publisher = "PLEIADES PUBLISHING INC",

number = "2",

}

RIS

TY - JOUR

T1 - Middle Paleozoic Rhyolite of the Gorny and Rudny Altai

T2 - Geochronology and Composition

AU - Kuibida, M. L.

AU - Timkin, V. I.

AU - Krivchikov, V. A.

AU - Murzin, O. V.

AU - Krupchatnikov, V. I.

AU - Popova, O. M.

AU - Kruk, N. N.

AU - Rudnev, S. N.

AU - Kuibida, Y. V.

AU - Shokal’sky, S. P.

AU - Gusev, N. I.

AU - Komiya, T.

AU - Aoki, S.

AU - Sun, M.

AU - Naryzhnova, A. V.

PY - 2019/8/1

Y1 - 2019/8/1

N2 - Abstract: The paper reports the results of geological, geochemical, and isotope–geochronological studies of subvolcanic rhyolites of NW Gorny Altai and Rudny Altai, which belong to the large Hercynian volcanic systems: Altai-Minusa and Altai–Salair, respectively. U–Pb zircon dating revealed two age groups: ~410–405 and 390–381 Ma. The isotope–geochemical characteristics of the rhyolites demonstrate high εNd(Т) from +2.6 to 6.0 with relatively young model ages T(DM) = 851–966 Ma in Rudny Altai and older model ages, up to 1266 Ma, in NW Gorny Altai. The rhyolites show transitional geochemical signatures between within-plate and island-arc felsic magmas. The results obtained are consistent with two-stage evolution of volcanism and its migration from the continent to the ocean.

AB - Abstract: The paper reports the results of geological, geochemical, and isotope–geochronological studies of subvolcanic rhyolites of NW Gorny Altai and Rudny Altai, which belong to the large Hercynian volcanic systems: Altai-Minusa and Altai–Salair, respectively. U–Pb zircon dating revealed two age groups: ~410–405 and 390–381 Ma. The isotope–geochemical characteristics of the rhyolites demonstrate high εNd(Т) from +2.6 to 6.0 with relatively young model ages T(DM) = 851–966 Ma in Rudny Altai and older model ages, up to 1266 Ma, in NW Gorny Altai. The rhyolites show transitional geochemical signatures between within-plate and island-arc felsic magmas. The results obtained are consistent with two-stage evolution of volcanism and its migration from the continent to the ocean.

KW - AGE

UR - http://www.scopus.com/inward/record.url?scp=85073242740&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19080130

DO - 10.1134/S1028334X19080130

M3 - Article

AN - SCOPUS:85073242740

VL - 487

SP - 885

EP - 889

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 21858358