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