Manifestation of Paleotsunami on the coast of primorye in the Holocene

Standard

Manifestation of Paleotsunami on the coast of primorye in the Holocene. / Ganzey, L. A.; Razzhigaeva, N. G.; Arslanov, Kh A.; Nishimura, Yu; Grebennikova, T. A.; Gorbunov, A. O.; Maksimov, F. E.; Petrov, A. Yu; Kharlamov, A. A.

In: Geomorfologiya, Vol. 2018-January, No. 2, 2018, p. 20-31.

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

Harvard

Ganzey, LA, Razzhigaeva, NG, Arslanov, KA, Nishimura, Y, Grebennikova, TA, Gorbunov, AO, Maksimov, FE, Petrov, AY & Kharlamov, AA 2018, 'Manifestation of Paleotsunami on the coast of primorye in the Holocene', Geomorfologiya, vol. 2018-January, no. 2, pp. 20-31. https://doi.org/10.7868/S0435428118020025

APA

Ganzey, L. A., Razzhigaeva, N. G., Arslanov, K. A., Nishimura, Y., Grebennikova, T. A., Gorbunov, A. O., Maksimov, F. E., Petrov, A. Y., & Kharlamov, A. A. (2018). Manifestation of Paleotsunami on the coast of primorye in the Holocene. Geomorfologiya, 2018-January(2), 20-31. https://doi.org/10.7868/S0435428118020025

Vancouver

Ganzey LA, Razzhigaeva NG, Arslanov KA, Nishimura Y, Grebennikova TA, Gorbunov AO et al. Manifestation of Paleotsunami on the coast of primorye in the Holocene. Geomorfologiya. 2018;2018-January(2):20-31. https://doi.org/10.7868/S0435428118020025

Author

Ganzey, L. A. ; Razzhigaeva, N. G. ; Arslanov, Kh A. ; Nishimura, Yu ; Grebennikova, T. A. ; Gorbunov, A. O. ; Maksimov, F. E. ; Petrov, A. Yu ; Kharlamov, A. A. / Manifestation of Paleotsunami on the coast of primorye in the Holocene. In: Geomorfologiya. 2018 ; Vol. 2018-January, No. 2. pp. 20-31.

BibTeX

@article{7a55dd75e5214e288e2ca5dff8dde6e3,

title = "Manifestation of Paleotsunami on the coast of primorye in the Holocene",

abstract = "The manifestation of strong tsunami in historical time and in the Late Holocene was revealed in the deposits of coastal lowlands along the seacoast of the Eastern and Southern Primorye (from Udobnaya Bay to Anna Bay and Russian Island), the Sea of Japan, the Russian Far East. The lithological methods and diatom analysis were used for identifying of tsunamigenic deposits. The sources of the material and the parameters of the tsunami were estimated for different bays. Determination of the age of the events was based on radiocarbon dating of hosting organogenic deposits and tephrostratigraphy. The correlation of events was made between individual sections, and the results were compared with paleotsunami data over the region. It was found that in the Sea of Japan coasts, large tsunami occur every 200 years, though the situations of shorter recurrence interval for strong tsunami can not be excluded also.",

keywords = "Coastal lowlands, Holocene, Paleotsunami deposits, Sea of Japan",

author = "Ganzey, {L. A.} and Razzhigaeva, {N. G.} and Arslanov, {Kh A.} and Yu Nishimura and Grebennikova, {T. A.} and Gorbunov, {A. O.} and Maksimov, {F. E.} and Petrov, {A. Yu} and Kharlamov, {A. A.}",

year = "2018",

doi = "10.7868/S0435428118020025",

language = "русский",

volume = "2018-January",

pages = "20--31",

journal = "ГЕОМОРФОЛОГИЯ",

issn = "0435-4281",

publisher = "Российская академия наук",

number = "2",

}

RIS

TY - JOUR

T1 - Manifestation of Paleotsunami on the coast of primorye in the Holocene

AU - Ganzey, L. A.

AU - Razzhigaeva, N. G.

AU - Arslanov, Kh A.

AU - Nishimura, Yu

AU - Grebennikova, T. A.

AU - Gorbunov, A. O.

AU - Maksimov, F. E.

AU - Petrov, A. Yu

AU - Kharlamov, A. A.

PY - 2018

Y1 - 2018

N2 - The manifestation of strong tsunami in historical time and in the Late Holocene was revealed in the deposits of coastal lowlands along the seacoast of the Eastern and Southern Primorye (from Udobnaya Bay to Anna Bay and Russian Island), the Sea of Japan, the Russian Far East. The lithological methods and diatom analysis were used for identifying of tsunamigenic deposits. The sources of the material and the parameters of the tsunami were estimated for different bays. Determination of the age of the events was based on radiocarbon dating of hosting organogenic deposits and tephrostratigraphy. The correlation of events was made between individual sections, and the results were compared with paleotsunami data over the region. It was found that in the Sea of Japan coasts, large tsunami occur every 200 years, though the situations of shorter recurrence interval for strong tsunami can not be excluded also.

AB - The manifestation of strong tsunami in historical time and in the Late Holocene was revealed in the deposits of coastal lowlands along the seacoast of the Eastern and Southern Primorye (from Udobnaya Bay to Anna Bay and Russian Island), the Sea of Japan, the Russian Far East. The lithological methods and diatom analysis were used for identifying of tsunamigenic deposits. The sources of the material and the parameters of the tsunami were estimated for different bays. Determination of the age of the events was based on radiocarbon dating of hosting organogenic deposits and tephrostratigraphy. The correlation of events was made between individual sections, and the results were compared with paleotsunami data over the region. It was found that in the Sea of Japan coasts, large tsunami occur every 200 years, though the situations of shorter recurrence interval for strong tsunami can not be excluded also.

KW - Coastal lowlands

KW - Holocene

KW - Paleotsunami deposits

KW - Sea of Japan

UR - http://www.scopus.com/inward/record.url?scp=85056535524&partnerID=8YFLogxK

U2 - 10.7868/S0435428118020025

DO - 10.7868/S0435428118020025

M3 - статья

AN - SCOPUS:85056535524

VL - 2018-January

SP - 20

EP - 31

JO - ГЕОМОРФОЛОГИЯ

JF - ГЕОМОРФОЛОГИЯ

SN - 0435-4281

IS - 2

ER -

ID: 89241472