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Discovery of Upper Oligocene–Lower Miocene brown coal deposits (Kosh-Agach formation) in the Dzhazator River valley (Southeastern Russian Altai) : Neotectonic and paleogeographical aspects. / Agatova, A. R.; Nepop, R. K.; Rudaya, N. A. et al.

In: Doklady Earth Sciences, Vol. 475, No. 2, 01.08.2017, p. 854-857.

Research output: Contribution to journalArticlepeer-review

Harvard

Agatova, AR, Nepop, RK, Rudaya, NA, Khazina, IV, Zhdanova, AN, Bronnikova, MA, Uspenskaya, ON, Zazovskaya, EP, Ovchinnikov, IY, Panov, VS & Shurygin, BN 2017, 'Discovery of Upper Oligocene–Lower Miocene brown coal deposits (Kosh-Agach formation) in the Dzhazator River valley (Southeastern Russian Altai): Neotectonic and paleogeographical aspects', Doklady Earth Sciences, vol. 475, no. 2, pp. 854-857. https://doi.org/10.1134/S1028334X17080104

APA

Agatova, A. R., Nepop, R. K., Rudaya, N. A., Khazina, I. V., Zhdanova, A. N., Bronnikova, M. A., Uspenskaya, O. N., Zazovskaya, E. P., Ovchinnikov, I. Y., Panov, V. S., & Shurygin, B. N. (2017). Discovery of Upper Oligocene–Lower Miocene brown coal deposits (Kosh-Agach formation) in the Dzhazator River valley (Southeastern Russian Altai): Neotectonic and paleogeographical aspects. Doklady Earth Sciences, 475(2), 854-857. https://doi.org/10.1134/S1028334X17080104

Vancouver

Agatova AR, Nepop RK, Rudaya NA, Khazina IV, Zhdanova AN, Bronnikova MA et al. Discovery of Upper Oligocene–Lower Miocene brown coal deposits (Kosh-Agach formation) in the Dzhazator River valley (Southeastern Russian Altai): Neotectonic and paleogeographical aspects. Doklady Earth Sciences. 2017 Aug 1;475(2):854-857. doi: 10.1134/S1028334X17080104

Author

BibTeX

@article{5688257d6ea242979fc27a903d4b9b97,
title = "Discovery of Upper Oligocene–Lower Miocene brown coal deposits (Kosh-Agach formation) in the Dzhazator River valley (Southeastern Russian Altai): Neotectonic and paleogeographical aspects",
abstract = "Results of complex paleontological and geochemical analysis are reported for a new locality of the Upper Oligocene–Lower Miocene Kosh-Agach carbonaceous formation in the Dzhazator River valley. This find specifies the scales of lacustrine–marsh sedimentation at the end of the Paleogene and beginning of the Neogene, as well as the character and amplitude of post-Neogene neotectonic movements in the southeastern highest mountain part of Russian Altai. Systematic rejuvenation of the radiocarbon age of the sequences studied, which has been established for the first time in Altai, is related to influx of young carbon during the subsequent complex geological history. This fact is of great importance for deciphering the chronology of Pleistocene glacial–dammed lakes in the intermontane basins of Altai and Tuva, the erosion zone of which spanned exhumed Tertiary deposits.",
author = "Agatova, {A. R.} and Nepop, {R. K.} and Rudaya, {N. A.} and Khazina, {I. V.} and Zhdanova, {A. N.} and Bronnikova, {M. A.} and Uspenskaya, {O. N.} and Zazovskaya, {E. P.} and Ovchinnikov, {I. Y.} and Panov, {V. S.} and Shurygin, {B. N.}",
year = "2017",
month = aug,
day = "1",
doi = "10.1134/S1028334X17080104",
language = "English",
volume = "475",
pages = "854--857",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Discovery of Upper Oligocene–Lower Miocene brown coal deposits (Kosh-Agach formation) in the Dzhazator River valley (Southeastern Russian Altai)

T2 - Neotectonic and paleogeographical aspects

AU - Agatova, A. R.

AU - Nepop, R. K.

AU - Rudaya, N. A.

AU - Khazina, I. V.

AU - Zhdanova, A. N.

AU - Bronnikova, M. A.

AU - Uspenskaya, O. N.

AU - Zazovskaya, E. P.

AU - Ovchinnikov, I. Y.

AU - Panov, V. S.

AU - Shurygin, B. N.

PY - 2017/8/1

Y1 - 2017/8/1

N2 - Results of complex paleontological and geochemical analysis are reported for a new locality of the Upper Oligocene–Lower Miocene Kosh-Agach carbonaceous formation in the Dzhazator River valley. This find specifies the scales of lacustrine–marsh sedimentation at the end of the Paleogene and beginning of the Neogene, as well as the character and amplitude of post-Neogene neotectonic movements in the southeastern highest mountain part of Russian Altai. Systematic rejuvenation of the radiocarbon age of the sequences studied, which has been established for the first time in Altai, is related to influx of young carbon during the subsequent complex geological history. This fact is of great importance for deciphering the chronology of Pleistocene glacial–dammed lakes in the intermontane basins of Altai and Tuva, the erosion zone of which spanned exhumed Tertiary deposits.

AB - Results of complex paleontological and geochemical analysis are reported for a new locality of the Upper Oligocene–Lower Miocene Kosh-Agach carbonaceous formation in the Dzhazator River valley. This find specifies the scales of lacustrine–marsh sedimentation at the end of the Paleogene and beginning of the Neogene, as well as the character and amplitude of post-Neogene neotectonic movements in the southeastern highest mountain part of Russian Altai. Systematic rejuvenation of the radiocarbon age of the sequences studied, which has been established for the first time in Altai, is related to influx of young carbon during the subsequent complex geological history. This fact is of great importance for deciphering the chronology of Pleistocene glacial–dammed lakes in the intermontane basins of Altai and Tuva, the erosion zone of which spanned exhumed Tertiary deposits.

UR - http://www.scopus.com/inward/record.url?scp=85028748153&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17080104

DO - 10.1134/S1028334X17080104

M3 - Article

AN - SCOPUS:85028748153

VL - 475

SP - 854

EP - 857

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 9915791