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Litogeochemistry of meso- and neoproterozoic terrigenios rocks of the southeast anabar basin : Evolution of source rocks and epigenetic alteration. / Kuptsova, A. V.; Khudoley, A. K.; Molchanov, A. V.

In: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, Vol. 2011, No. 7, 01.12.2011, p. 17-31.

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

Harvard

Kuptsova, AV, Khudoley, AK & Molchanov, AV 2011, 'Litogeochemistry of meso- and neoproterozoic terrigenios rocks of the southeast anabar basin: Evolution of source rocks and epigenetic alteration', ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, vol. 2011, no. 7, pp. 17-31.

APA

Kuptsova, A. V., Khudoley, A. K., & Molchanov, A. V. (2011). Litogeochemistry of meso- and neoproterozoic terrigenios rocks of the southeast anabar basin: Evolution of source rocks and epigenetic alteration. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ, 2011(7), 17-31.

Vancouver

Kuptsova AV, Khudoley AK, Molchanov AV. Litogeochemistry of meso- and neoproterozoic terrigenios rocks of the southeast anabar basin: Evolution of source rocks and epigenetic alteration. ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2011 Dec 1;2011(7):17-31.

Author

Kuptsova, A. V. ; Khudoley, A. K. ; Molchanov, A. V. / Litogeochemistry of meso- and neoproterozoic terrigenios rocks of the southeast anabar basin : Evolution of source rocks and epigenetic alteration. In: ВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ. 2011 ; Vol. 2011, No. 7. pp. 17-31.

BibTeX

@article{19ec9a86e10442b295695e3684e442cc,
title = "Litogeochemistry of meso- and neoproterozoic terrigenios rocks of the southeast anabar basin: Evolution of source rocks and epigenetic alteration",
abstract = "The paper describes Meso- and Neoproterozoic rocks from the south part of the East-Anabar Basin. Based on lithological, isotopic and geochemical datawe established that provenance area included predominantly metamorphic rocks of the Anabar Shield. The formation of Riphean sandstones and conglomerates was related to erosion of Daldyn terrane. At the beginning of Vendian time the provenance area was displaced eastward and included Birecte granite-greenstone terrane. Hydrothermal alteration is supposed to be Mesozoic.",
keywords = "East-Anabar Basin, Geochemistry, Meso- and Neoproterozoic, Provenance, Sm-Nd study",
author = "Kuptsova, {A. V.} and Khudoley, {A. K.} and Molchanov, {A. V.}",
year = "2011",
month = dec,
day = "1",
language = "English",
volume = "2011",
pages = "17--31",
journal = "Вестник Санкт-Петербургского университета. Науки о Земле",
issn = "1812-9323",
publisher = "Издательство Санкт-Петербургского университета",
number = "7",

}

RIS

TY - JOUR

T1 - Litogeochemistry of meso- and neoproterozoic terrigenios rocks of the southeast anabar basin

T2 - Evolution of source rocks and epigenetic alteration

AU - Kuptsova, A. V.

AU - Khudoley, A. K.

AU - Molchanov, A. V.

PY - 2011/12/1

Y1 - 2011/12/1

N2 - The paper describes Meso- and Neoproterozoic rocks from the south part of the East-Anabar Basin. Based on lithological, isotopic and geochemical datawe established that provenance area included predominantly metamorphic rocks of the Anabar Shield. The formation of Riphean sandstones and conglomerates was related to erosion of Daldyn terrane. At the beginning of Vendian time the provenance area was displaced eastward and included Birecte granite-greenstone terrane. Hydrothermal alteration is supposed to be Mesozoic.

AB - The paper describes Meso- and Neoproterozoic rocks from the south part of the East-Anabar Basin. Based on lithological, isotopic and geochemical datawe established that provenance area included predominantly metamorphic rocks of the Anabar Shield. The formation of Riphean sandstones and conglomerates was related to erosion of Daldyn terrane. At the beginning of Vendian time the provenance area was displaced eastward and included Birecte granite-greenstone terrane. Hydrothermal alteration is supposed to be Mesozoic.

KW - East-Anabar Basin

KW - Geochemistry

KW - Meso- and Neoproterozoic

KW - Provenance

KW - Sm-Nd study

UR - http://www.scopus.com/inward/record.url?scp=84859413932&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:84859413932

VL - 2011

SP - 17

EP - 31

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 1812-9323

IS - 7

ER -

ID: 43293107