Mesozoic–Cenozoic Evolution and the Fault Kinematics of the Nurol Depression (Southern West Siberian Basin)

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Mesozoic–Cenozoic Evolution and the Fault Kinematics of the Nurol Depression (Southern West Siberian Basin). / Moskalenko, A. N.; Khudoley, A. K.

в: Doklady Earth Sciences, Том 493, № 2, 21.09.2020, стр. 589-592.

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

BibTeX

@article{9de84c1646ce4cc984cda0da1021cfff,

title = "Mesozoic–Cenozoic Evolution and the Fault Kinematics of the Nurol Depression (Southern West Siberian Basin)",

abstract = "Abstract: New fault kinematics data within the Archinsk field located in the Nurol depression (south part of the West Siberian Basin) are obtained by structural analysis of the 3D seismic reflection data. Two stages of fault formation in the Mesozoic–Cenozoic period are distinguished. The first stage is characterized by a normal stress regime with a NE-trending minimum principal stress and corresponds to Triassic rifting. The second stage is characterized by Cenozoic reactivation of the pre-existing faults and the formation of new, predominantly strike-slip faults, with submeridionally and sublatitudinally trending minimum and maximum principal stresses, respectively.",

keywords = "fault kinematics analysis, Nurol depression, seismic data, stress field, structural analysis, West Siberian Basin",

author = "Moskalenko, {A. N.} and Khudoley, {A. K.}",

note = "Publisher Copyright: {\textcopyright} 2020, Pleiades Publishing, Ltd.",

year = "2020",

month = sep,

day = "21",

doi = "10.1134/S1028334X20080152",

language = "English",

volume = "493",

pages = "589--592",

journal = "Doklady Earth Sciences",

issn = "1028-334X",

publisher = "МАИК {"}Наука/Интерпериодика{"}",

number = "2",

}

RIS

TY - JOUR

T1 - Mesozoic–Cenozoic Evolution and the Fault Kinematics of the Nurol Depression (Southern West Siberian Basin)

AU - Moskalenko, A. N.

AU - Khudoley, A. K.

PY - 2020/9/21

Y1 - 2020/9/21

N2 - Abstract: New fault kinematics data within the Archinsk field located in the Nurol depression (south part of the West Siberian Basin) are obtained by structural analysis of the 3D seismic reflection data. Two stages of fault formation in the Mesozoic–Cenozoic period are distinguished. The first stage is characterized by a normal stress regime with a NE-trending minimum principal stress and corresponds to Triassic rifting. The second stage is characterized by Cenozoic reactivation of the pre-existing faults and the formation of new, predominantly strike-slip faults, with submeridionally and sublatitudinally trending minimum and maximum principal stresses, respectively.

AB - Abstract: New fault kinematics data within the Archinsk field located in the Nurol depression (south part of the West Siberian Basin) are obtained by structural analysis of the 3D seismic reflection data. Two stages of fault formation in the Mesozoic–Cenozoic period are distinguished. The first stage is characterized by a normal stress regime with a NE-trending minimum principal stress and corresponds to Triassic rifting. The second stage is characterized by Cenozoic reactivation of the pre-existing faults and the formation of new, predominantly strike-slip faults, with submeridionally and sublatitudinally trending minimum and maximum principal stresses, respectively.

KW - fault kinematics analysis

KW - Nurol depression

KW - seismic data

KW - stress field

KW - structural analysis

KW - West Siberian Basin

UR - http://www.scopus.com/inward/record.url?scp=85091252224&partnerID=8YFLogxK

U2 - 10.1134/S1028334X20080152

DO - 10.1134/S1028334X20080152

M3 - Article

AN - SCOPUS:85091252224

VL - 493

SP - 589

EP - 592

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 89180593