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On a Discussion on the Correlation of the Bajocian–Bathonian Sections in the Izhma River Basin, European North of Russia. / Mitta, V. V.; Glinskikh, L. A.; Kostyleva, V. V. et al.

In: Stratigraphy and Geological Correlation, Vol. 30, 2022, p. S96-S108.

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Mitta VV, Glinskikh LA, Kostyleva VV, Shurygin BN, Dzyuba OS, Nikitenko BL. On a Discussion on the Correlation of the Bajocian–Bathonian Sections in the Izhma River Basin, European North of Russia. Stratigraphy and Geological Correlation. 2022;30:S96-S108. doi: 10.1134/S0869593823010069

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Mitta, V. V. ; Glinskikh, L. A. ; Kostyleva, V. V. et al. / On a Discussion on the Correlation of the Bajocian–Bathonian Sections in the Izhma River Basin, European North of Russia. In: Stratigraphy and Geological Correlation. 2022 ; Vol. 30. pp. S96-S108.

BibTeX

@article{8c19110d982e473183b6a38e9233232e,
title = "On a Discussion on the Correlation of the Bajocian–Bathonian Sections in the Izhma River Basin, European North of Russia",
abstract = "In the Izhma River basin, the Upper Bajocian–Lower Bathonian sections crop out at several localities along the Dreshchanka River. A recently published opinion (Ippolitov, A.P., Kiselev, D.N. “Geological Features of the Bajocian–Bathonian in the Reference Section of the Izhma River Basin (North of European Russia) and the Succession of Ammonites of the Subfamily Arctocephalitinae Meledina,” Stratigraphy and Geological Correlation, 2021, vol. 29, pp. 742–755) on the correlation of these sections, as well as the comments made in the same paper on the results of our research, are critically reviewed. The correlation model constructed using the strato-isohypses of the top of the Arcticoceras-bearing sandstone horizon, constructed by Ippolitov and Kiselev relative to four marks of the water level, turned out to be factually unfounded and methodologically unsubstantiated. Arguments against this model are as follows: the low efficiency of the interpolation method on a small sample size when constructing the riverbed dip profile under conditions of intensive meandering of the Dreshchanka River on the floodplain terrace; ignoring the geomorphological situation as a whole; the irrelevance of the topographic map of the 1999 edition; the underestimation of the variability of the low-water position of the water level in different years due to changes in the amount of precipitation.",
keywords = "Lower Bathonian, Pechorian North, Upper Bajocian, stratigraphy",
author = "Mitta, {V. V.} and Glinskikh, {L. A.} and Kostyleva, {V. V.} and Shurygin, {B. N.} and Dzyuba, {O. S.} and Nikitenko, {B. L.}",
note = "Публикация для корректировки.",
year = "2022",
doi = "10.1134/S0869593823010069",
language = "English",
volume = "30",
pages = "S96--S108",
journal = "Stratigraphy and Geological Correlation",
issn = "0869-5938",
publisher = "PLEIADES PUBLISHING INC",

}

RIS

TY - JOUR

T1 - On a Discussion on the Correlation of the Bajocian–Bathonian Sections in the Izhma River Basin, European North of Russia

AU - Mitta, V. V.

AU - Glinskikh, L. A.

AU - Kostyleva, V. V.

AU - Shurygin, B. N.

AU - Dzyuba, O. S.

AU - Nikitenko, B. L.

N1 - Публикация для корректировки.

PY - 2022

Y1 - 2022

N2 - In the Izhma River basin, the Upper Bajocian–Lower Bathonian sections crop out at several localities along the Dreshchanka River. A recently published opinion (Ippolitov, A.P., Kiselev, D.N. “Geological Features of the Bajocian–Bathonian in the Reference Section of the Izhma River Basin (North of European Russia) and the Succession of Ammonites of the Subfamily Arctocephalitinae Meledina,” Stratigraphy and Geological Correlation, 2021, vol. 29, pp. 742–755) on the correlation of these sections, as well as the comments made in the same paper on the results of our research, are critically reviewed. The correlation model constructed using the strato-isohypses of the top of the Arcticoceras-bearing sandstone horizon, constructed by Ippolitov and Kiselev relative to four marks of the water level, turned out to be factually unfounded and methodologically unsubstantiated. Arguments against this model are as follows: the low efficiency of the interpolation method on a small sample size when constructing the riverbed dip profile under conditions of intensive meandering of the Dreshchanka River on the floodplain terrace; ignoring the geomorphological situation as a whole; the irrelevance of the topographic map of the 1999 edition; the underestimation of the variability of the low-water position of the water level in different years due to changes in the amount of precipitation.

AB - In the Izhma River basin, the Upper Bajocian–Lower Bathonian sections crop out at several localities along the Dreshchanka River. A recently published opinion (Ippolitov, A.P., Kiselev, D.N. “Geological Features of the Bajocian–Bathonian in the Reference Section of the Izhma River Basin (North of European Russia) and the Succession of Ammonites of the Subfamily Arctocephalitinae Meledina,” Stratigraphy and Geological Correlation, 2021, vol. 29, pp. 742–755) on the correlation of these sections, as well as the comments made in the same paper on the results of our research, are critically reviewed. The correlation model constructed using the strato-isohypses of the top of the Arcticoceras-bearing sandstone horizon, constructed by Ippolitov and Kiselev relative to four marks of the water level, turned out to be factually unfounded and methodologically unsubstantiated. Arguments against this model are as follows: the low efficiency of the interpolation method on a small sample size when constructing the riverbed dip profile under conditions of intensive meandering of the Dreshchanka River on the floodplain terrace; ignoring the geomorphological situation as a whole; the irrelevance of the topographic map of the 1999 edition; the underestimation of the variability of the low-water position of the water level in different years due to changes in the amount of precipitation.

KW - Lower Bathonian

KW - Pechorian North

KW - Upper Bajocian

KW - stratigraphy

UR - https://www.mendeley.com/catalogue/4cd5d7e6-41ab-3d12-8ac0-53ec95d087fb/

U2 - 10.1134/S0869593823010069

DO - 10.1134/S0869593823010069

M3 - Article

VL - 30

SP - S96-S108

JO - Stratigraphy and Geological Correlation

JF - Stratigraphy and Geological Correlation

SN - 0869-5938

ER -

ID: 55694581