Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
The Basal Unit of the Verkhoyansk Sedimentary Complex, Northern Kharaulakh: Lithostratigraphy, Biostratigraphy, and Deposition Environments. / Sennikov, N.; Khabibulina, R. A.; Gonta, T. и др.
в: Russian Geology and Geophysics, Том 61, № 12, 12.2020, стр. 1391-1411.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - The Basal Unit of the Verkhoyansk Sedimentary Complex, Northern Kharaulakh: Lithostratigraphy, Biostratigraphy, and Deposition Environments
AU - Sennikov, N.
AU - Khabibulina, R. A.
AU - Gonta, T.
AU - Obut, O. T.
N1 - Funding Information: The study was supported by grant 18-05-70035 from the Russian Foundation for Basic Research. Publisher Copyright: © 2020, V.S. Sobolev IGM, Siberian Branch of the RAS.
PY - 2020/12
Y1 - 2020/12
N2 - The origin and biostratigraphic constraints of the Krestyakh conglomerate remain among most controversial issues in the Late Paleozoic history of the Northern Kharaulakh basin. The Krestyakh conglomerate is a sequence of coarse sand to pebble-size sediments at the base of the Late Paleozoic Verkhoyansk clastic complex. According to geological, lithological, and sedimentation data, the Krestyakh conglomerate in the Atyrdakh Formation is composed of debrites i.e., deposits carried by debris flows that fill submarine canyons. The Verkhoyansk clastic deposition began at the middle Visean stage of the Early Carboniferous.
AB - The origin and biostratigraphic constraints of the Krestyakh conglomerate remain among most controversial issues in the Late Paleozoic history of the Northern Kharaulakh basin. The Krestyakh conglomerate is a sequence of coarse sand to pebble-size sediments at the base of the Late Paleozoic Verkhoyansk clastic complex. According to geological, lithological, and sedimentation data, the Krestyakh conglomerate in the Atyrdakh Formation is composed of debrites i.e., deposits carried by debris flows that fill submarine canyons. The Verkhoyansk clastic deposition began at the middle Visean stage of the Early Carboniferous.
KW - Carboniferous
KW - Visean
KW - stratigraphy
KW - lithology
KW - Northern Kharaulakh
KW - LENA RIVER
UR - http://www.scopus.com/inward/record.url?scp=85121686982&partnerID=8YFLogxK
U2 - 10.15372/RGG2020138
DO - 10.15372/RGG2020138
M3 - Article
VL - 61
SP - 1391
EP - 1411
JO - Russian Geology and Geophysics
JF - Russian Geology and Geophysics
SN - 1068-7971
IS - 12
ER -
ID: 27354066