Jurassic and Cretaceous stratigraphy of the New Siberian Archipelago (Laptev and East Siberian Seas)

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Jurassic and Cretaceous stratigraphy of the New Siberian Archipelago (Laptev and East Siberian Seas) : facies zoning and lithostratigraphy. / Nikitenko, B. L.; Devyatov, V. P.; Lebedeva, N. K. et al.

In: Russian Geology and Geophysics, Vol. 58, No. 12, 01.12.2017, p. 1478-1493.

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

BibTeX

@article{332fe9e743914f669429919389602973,

title = "Jurassic and Cretaceous stratigraphy of the New Siberian Archipelago (Laptev and East Siberian Seas): facies zoning and lithostratigraphy",

abstract = "Mesozoic sections in the New Siberian Archipelago are important for understanding of the geology of underexplored shelf areas in the east of the Laptev Sea and in the west of the East Siberian Sea. They are reference sections for interpretation of seismic data in these regions. However, there are still many unresolved problems concerning the lithology, lateral extent, and age of Mesozoic deposits, as the sections have a complex structure and are heavily deformed. The performed research makes a basis for the first facies zoning of Jurassic and Cretaceous deposits in the New Siberian Islands and adjacent landmasses of continental Siberia at the junction of the Laptev and East Siberian Seas. The lithostratigraphic division of the Jurassic and Cretaceous is refined, being proposed for the first time for some stratigraphic intervals, and allows updating their lithostratigraphic division (or undertaking it for the first time for some stratigraphic intervals). Facies features of Jurassic and Cretaceous deposits allow the definition of three depositional series.",

keywords = "Arctic, Cretaceous, dinoflagellate cysts, Dummy Introduction, facies division, foraminifera, Jurassic, New Siberian Islands, ostracods, spores and pollen, stratigraphy, SEDIMENTS, STOLBOVOI-ISLAND",

author = "Nikitenko, {B. L.} and Devyatov, {V. P.} and Lebedeva, {N. K.} and Basov, {V. A.} and Goryacheva, {A. A.} and Pestchevitskaya, {E. B.} and Glinskikh, {L. A.}",

note = "Publisher Copyright: {\textcopyright} 2017",

year = "2017",

month = dec,

day = "1",

doi = "10.1016/j.rgg.2017.11.012",

language = "English",

volume = "58",

pages = "1478--1493",

journal = "Russian Geology and Geophysics",

issn = "1068-7971",

publisher = "Elsevier Science B.V.",

number = "12",

}

RIS

TY - JOUR

T1 - Jurassic and Cretaceous stratigraphy of the New Siberian Archipelago (Laptev and East Siberian Seas)

T2 - facies zoning and lithostratigraphy

AU - Nikitenko, B. L.

AU - Devyatov, V. P.

AU - Lebedeva, N. K.

AU - Basov, V. A.

AU - Goryacheva, A. A.

AU - Pestchevitskaya, E. B.

AU - Glinskikh, L. A.

PY - 2017/12/1

Y1 - 2017/12/1

N2 - Mesozoic sections in the New Siberian Archipelago are important for understanding of the geology of underexplored shelf areas in the east of the Laptev Sea and in the west of the East Siberian Sea. They are reference sections for interpretation of seismic data in these regions. However, there are still many unresolved problems concerning the lithology, lateral extent, and age of Mesozoic deposits, as the sections have a complex structure and are heavily deformed. The performed research makes a basis for the first facies zoning of Jurassic and Cretaceous deposits in the New Siberian Islands and adjacent landmasses of continental Siberia at the junction of the Laptev and East Siberian Seas. The lithostratigraphic division of the Jurassic and Cretaceous is refined, being proposed for the first time for some stratigraphic intervals, and allows updating their lithostratigraphic division (or undertaking it for the first time for some stratigraphic intervals). Facies features of Jurassic and Cretaceous deposits allow the definition of three depositional series.

AB - Mesozoic sections in the New Siberian Archipelago are important for understanding of the geology of underexplored shelf areas in the east of the Laptev Sea and in the west of the East Siberian Sea. They are reference sections for interpretation of seismic data in these regions. However, there are still many unresolved problems concerning the lithology, lateral extent, and age of Mesozoic deposits, as the sections have a complex structure and are heavily deformed. The performed research makes a basis for the first facies zoning of Jurassic and Cretaceous deposits in the New Siberian Islands and adjacent landmasses of continental Siberia at the junction of the Laptev and East Siberian Seas. The lithostratigraphic division of the Jurassic and Cretaceous is refined, being proposed for the first time for some stratigraphic intervals, and allows updating their lithostratigraphic division (or undertaking it for the first time for some stratigraphic intervals). Facies features of Jurassic and Cretaceous deposits allow the definition of three depositional series.

KW - Arctic

KW - Cretaceous

KW - dinoflagellate cysts

KW - Dummy Introduction

KW - facies division

KW - foraminifera

KW - Jurassic

KW - New Siberian Islands

KW - ostracods

KW - spores and pollen

KW - stratigraphy

KW - SEDIMENTS

KW - STOLBOVOI-ISLAND

UR - http://www.scopus.com/inward/record.url?scp=85037043001&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2017.11.012

DO - 10.1016/j.rgg.2017.11.012

M3 - Article

AN - SCOPUS:85037043001

VL - 58

SP - 1478

EP - 1493

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 12

ER -

ID: 9647406

Jurassic and Cretaceous stratigraphy of the New Siberian Archipelago (Laptev and East Siberian Seas): facies zoning and lithostratigraphy

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