Distribution of Cambrian salts in the western Siberian craton (Yurubcheno-Tokhomo field, Russia)

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Distribution of Cambrian salts in the western Siberian craton (Yurubcheno-Tokhomo field, Russia). / Novikov, Dmitry Anatolievich.

в: Arabian Journal of Geosciences, Том 10, № 1, 7, 01.01.2017.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

BibTeX

@article{233ac475378d4e7ab8d26dcfe93c3914,

title = "Distribution of Cambrian salts in the western Siberian craton (Yurubcheno-Tokhomo field, Russia)",

abstract = "An integrated logging and deep drilling data interpretation has provided insight to the section of the Yurubcheno-Tokhomo field. Five phases of salt deposition of 50–350 m in the cumulative thickness have been identified (top–bottom): upper Litvintsevo, Angara, upper Belsk, upper Usolye, and lower Usolye. Cumulative thickness of Cambrian salts was found to reach 550–600 m, with predominance of 1- to 9-m salt layers. In the Cambrian, the study area was a shallow warm basin of sabkha type and favored salt evaporation. Regression periods controlled the thicknesses of salts.",

keywords = "Cambrian, Geological model, Salt deposition, Siberian craton, PLATFORM, TECTONICS, CHINA, BASIN, PROVINCE, OMAN",

author = "Novikov, {Dmitry Anatolievich}",

note = "Publisher Copyright: {\textcopyright} 2016, Saudi Society for Geosciences.",

year = "2017",

month = jan,

day = "1",

doi = "10.1007/s12517-016-2792-0",

language = "English",

volume = "10",

journal = "Arabian Journal of Geosciences",

issn = "1866-7511",

publisher = "Springer-Verlag GmbH and Co. KG",

number = "1",

}

RIS

TY - JOUR

T1 - Distribution of Cambrian salts in the western Siberian craton (Yurubcheno-Tokhomo field, Russia)

AU - Novikov, Dmitry Anatolievich

PY - 2017/1/1

Y1 - 2017/1/1

N2 - An integrated logging and deep drilling data interpretation has provided insight to the section of the Yurubcheno-Tokhomo field. Five phases of salt deposition of 50–350 m in the cumulative thickness have been identified (top–bottom): upper Litvintsevo, Angara, upper Belsk, upper Usolye, and lower Usolye. Cumulative thickness of Cambrian salts was found to reach 550–600 m, with predominance of 1- to 9-m salt layers. In the Cambrian, the study area was a shallow warm basin of sabkha type and favored salt evaporation. Regression periods controlled the thicknesses of salts.

AB - An integrated logging and deep drilling data interpretation has provided insight to the section of the Yurubcheno-Tokhomo field. Five phases of salt deposition of 50–350 m in the cumulative thickness have been identified (top–bottom): upper Litvintsevo, Angara, upper Belsk, upper Usolye, and lower Usolye. Cumulative thickness of Cambrian salts was found to reach 550–600 m, with predominance of 1- to 9-m salt layers. In the Cambrian, the study area was a shallow warm basin of sabkha type and favored salt evaporation. Regression periods controlled the thicknesses of salts.

KW - Cambrian

KW - Geological model

KW - Salt deposition

KW - Siberian craton

KW - PLATFORM

KW - TECTONICS

KW - CHINA

KW - BASIN

KW - PROVINCE

KW - OMAN

UR - http://www.scopus.com/inward/record.url?scp=85007460064&partnerID=8YFLogxK

U2 - 10.1007/s12517-016-2792-0

DO - 10.1007/s12517-016-2792-0

M3 - Article

AN - SCOPUS:85007460064

VL - 10

JO - Arabian Journal of Geosciences

JF - Arabian Journal of Geosciences

SN - 1866-7511

IS - 1

M1 - 7

ER -

ID: 10316917