Detrital zircons from the Albian sandstone of the Silasa and Kema formations (Sikhote—Alin Orogen): U—Pb age and geodynamic implications

A. N. Didenko; S. Otoh; V. V. Golozubov; M. V. Arkhipov; A. V. Kudymov; A. Yu Peskov; M. Nagata; K. Yamamoto

doi:10.1134/S1028334X18080032

Detrital zircons from the Albian sandstone of the Silasa and Kema formations (Sikhote—Alin Orogen): U—Pb age and geodynamic implications

A. N. Didenko, S. Otoh, V. V. Golozubov, M. V. Arkhipov^*, A. V. Kudymov, A. Yu Peskov, M. Nagata, K. Yamamoto

^*Corresponding author for this work

Earth System Science

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

5 Scopus citations

Abstract

New results of dating of detrital zircons from the Kema and Silasa Formations (Albian, Sikhote–Alin Orogenic Belt) permit determination of the provenance sources and geodynamic settings of sediment deposition. The Silasa Formation was deposited in outer island arc settings, separated by a forearc basin from the inner island arc, where the Kema Formation sediments were accumulated. The significant depth and width of the forearc basin hindered input of continent-derived debris to the area of sedimentation of the Silasa Formation.

Original language	English
Pages (from-to)	1000-1003
Number of pages	4
Journal	Doklady Earth Sciences
Volume	481
Issue number	2
DOIs	https://doi.org/10.1134/S1028334X18080032
State	Published - 2018/08/01

ASJC Scopus subject areas

Earth and Planetary Sciences (miscellaneous)
General Earth and Planetary Sciences

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title = "Detrital zircons from the Albian sandstone of the Silasa and Kema formations (Sikhote—Alin Orogen): U—Pb age and geodynamic implications",

abstract = "New results of dating of detrital zircons from the Kema and Silasa Formations (Albian, Sikhote–Alin Orogenic Belt) permit determination of the provenance sources and geodynamic settings of sediment deposition. The Silasa Formation was deposited in outer island arc settings, separated by a forearc basin from the inner island arc, where the Kema Formation sediments were accumulated. The significant depth and width of the forearc basin hindered input of continent-derived debris to the area of sedimentation of the Silasa Formation.",

author = "Didenko, {A. N.} and S. Otoh and Golozubov, {V. V.} and Arkhipov, {M. V.} and Kudymov, {A. V.} and Peskov, {A. Yu} and M. Nagata and K. Yamamoto",

note = "Publisher Copyright: {\textcopyright} 2018, Pleiades Publishing, Ltd.",

year = "2018",

month = aug,

day = "1",

doi = "10.1134/S1028334X18080032",

language = "英語",

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TY - JOUR

T1 - Detrital zircons from the Albian sandstone of the Silasa and Kema formations (Sikhote—Alin Orogen)

T2 - U—Pb age and geodynamic implications

AU - Didenko, A. N.

AU - Otoh, S.

AU - Golozubov, V. V.

AU - Arkhipov, M. V.

AU - Kudymov, A. V.

AU - Peskov, A. Yu

AU - Nagata, M.

AU - Yamamoto, K.

PY - 2018/8/1

Y1 - 2018/8/1

N2 - New results of dating of detrital zircons from the Kema and Silasa Formations (Albian, Sikhote–Alin Orogenic Belt) permit determination of the provenance sources and geodynamic settings of sediment deposition. The Silasa Formation was deposited in outer island arc settings, separated by a forearc basin from the inner island arc, where the Kema Formation sediments were accumulated. The significant depth and width of the forearc basin hindered input of continent-derived debris to the area of sedimentation of the Silasa Formation.

AB - New results of dating of detrital zircons from the Kema and Silasa Formations (Albian, Sikhote–Alin Orogenic Belt) permit determination of the provenance sources and geodynamic settings of sediment deposition. The Silasa Formation was deposited in outer island arc settings, separated by a forearc basin from the inner island arc, where the Kema Formation sediments were accumulated. The significant depth and width of the forearc basin hindered input of continent-derived debris to the area of sedimentation of the Silasa Formation.

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U2 - 10.1134/S1028334X18080032

DO - 10.1134/S1028334X18080032

M3 - 学術論文

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SN - 1028-334X

VL - 481

SP - 1000

EP - 1003

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

IS - 2

ER -

Detrital zircons from the Albian sandstone of the Silasa and Kema formations (Sikhote—Alin Orogen): U—Pb age and geodynamic implications

Abstract

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