The Basal Unit of the Verkhoyansk Sedimentary Complex, Northern Kharaulakh: Lithostratigraphy, Biostratigraphy, and Deposition Environments

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The Basal Unit of the Verkhoyansk Sedimentary Complex, Northern Kharaulakh: Lithostratigraphy, Biostratigraphy, and Deposition Environments. / Sennikov, N.; Khabibulina, R. A.; Gonta, T. et al.

In: Russian Geology and Geophysics, Vol. 61, No. 12, 12.2020, p. 1391-1411.

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

BibTeX

@article{624813c9786c42909bf59e4d3323377c,

title = "The Basal Unit of the Verkhoyansk Sedimentary Complex, Northern Kharaulakh: Lithostratigraphy, Biostratigraphy, and Deposition Environments",

abstract = "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.",

keywords = "Carboniferous, Visean, stratigraphy, lithology, Northern Kharaulakh, LENA RIVER",

author = "N. Sennikov and Khabibulina, {R. A.} and T. Gonta and Obut, {O. T.}",

note = "Funding Information: The study was supported by grant 18-05-70035 from the Russian Foundation for Basic Research. Publisher Copyright: {\textcopyright} 2020, V.S. Sobolev IGM, Siberian Branch of the RAS.",

year = "2020",

month = dec,

doi = "10.15372/RGG2020138",

language = "English",

volume = "61",

pages = "1391--1411",

journal = "Russian Geology and Geophysics",

issn = "1068-7971",

publisher = "Elsevier Science B.V.",

number = "12",

}

RIS

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.

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