SPATIAL VARIATIONS OF SEISMIC WAVE ATTENUATION IN THE SOUTH BAIKAL BASIN AND ADJACENT AREAS (BAIKAL RIFT)

Our detailed study of the crust and upper mantle of the South Baikal basin focused on seismic coda and seismic S-waves attenuation and estimated seismic quality factor (QS and QC), frequency parameter (n), attenuation coefficient (δ), total attenuation (QT), and the ratio of two components the total...
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Gespeichert in:

Autor*in:	A. A. Dobrynina [verfasserIn] P. A. Predein [verfasserIn] V. A. Sankov [verfasserIn] Ts. A. Tubanov [verfasserIn] D. P.-D. Sanzhieva [verfasserIn] E. A. Gorbunova [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch ; Russisch

Erschienen:	2019

Schlagwörter:	south baikal rift basin seismic quality factor attenuation seismic coda s-waves earthquake explosion block divisibility of the medium components of attenuation active fault

Übergeordnetes Werk:	In: Геодинамика и тектонофизика - Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust, 2015, 10(2019), 1, Seite 147-166
Übergeordnetes Werk:	volume:10 ; year:2019 ; number:1 ; pages:147-166

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.5800/GT-2019-10-1-0408

Katalog-ID:	DOAJ02181242X

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language	English Russian
source	In Геодинамика и тектонофизика 10(2019), 1, Seite 147-166 volume:10 year:2019 number:1 pages:147-166
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author	A. A. Dobrynina
spellingShingle	A. A. Dobrynina misc south baikal rift basin misc seismic quality factor misc attenuation misc seismic coda misc s-waves misc earthquake misc explosion misc block divisibility of the medium misc components of attenuation misc active fault misc Science misc Q SPATIAL VARIATIONS OF SEISMIC WAVE ATTENUATION IN THE SOUTH BAIKAL BASIN AND ADJACENT AREAS (BAIKAL RIFT)
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topic_title	SPATIAL VARIATIONS OF SEISMIC WAVE ATTENUATION IN THE SOUTH BAIKAL BASIN AND ADJACENT AREAS (BAIKAL RIFT) south baikal rift basin seismic quality factor attenuation seismic coda s-waves earthquake explosion block divisibility of the medium components of attenuation active fault
topic	misc south baikal rift basin misc seismic quality factor misc attenuation misc seismic coda misc s-waves misc earthquake misc explosion misc block divisibility of the medium misc components of attenuation misc active fault misc Science misc Q
topic_unstemmed	misc south baikal rift basin misc seismic quality factor misc attenuation misc seismic coda misc s-waves misc earthquake misc explosion misc block divisibility of the medium misc components of attenuation misc active fault misc Science misc Q
topic_browse	misc south baikal rift basin misc seismic quality factor misc attenuation misc seismic coda misc s-waves misc earthquake misc explosion misc block divisibility of the medium misc components of attenuation misc active fault misc Science misc Q
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title	SPATIAL VARIATIONS OF SEISMIC WAVE ATTENUATION IN THE SOUTH BAIKAL BASIN AND ADJACENT AREAS (BAIKAL RIFT)
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title_full	SPATIAL VARIATIONS OF SEISMIC WAVE ATTENUATION IN THE SOUTH BAIKAL BASIN AND ADJACENT AREAS (BAIKAL RIFT)
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title_sort	spatial variations of seismic wave attenuation in the south baikal basin and adjacent areas (baikal rift)
title_auth	SPATIAL VARIATIONS OF SEISMIC WAVE ATTENUATION IN THE SOUTH BAIKAL BASIN AND ADJACENT AREAS (BAIKAL RIFT)
abstract	Our detailed study of the crust and upper mantle of the South Baikal basin focused on seismic coda and seismic S-waves attenuation and estimated seismic quality factor (QS and QC), frequency parameter (n), attenuation coefficient (δ), total attenuation (QT), and the ratio of two components the total attenuation: intrinsic attenuation (Qi), and attenuation due to scattering caused by the inhomogeneities of the medium (QSC). We calculated the sizes of inhomogeneities revealed in the block medium, which put their effect on the attenuation of seismic waves in different frequency ranges. The seismic wave attenuation field was analyzed in comparison with the geological and geophysical characteristics of the medium, and a direct relationship was established between attenuation, composition and active processes in the crust and upper mantle of the studied area. According to the estimated intrinsic attenuation (Qi) and scattering attenuation (QSC) contributions into the total attenuation, intrinsic attenuation is generally dominant in the studied area, while the QSC component increases in the areas of large active faults.
abstractGer	Our detailed study of the crust and upper mantle of the South Baikal basin focused on seismic coda and seismic S-waves attenuation and estimated seismic quality factor (QS and QC), frequency parameter (n), attenuation coefficient (δ), total attenuation (QT), and the ratio of two components the total attenuation: intrinsic attenuation (Qi), and attenuation due to scattering caused by the inhomogeneities of the medium (QSC). We calculated the sizes of inhomogeneities revealed in the block medium, which put their effect on the attenuation of seismic waves in different frequency ranges. The seismic wave attenuation field was analyzed in comparison with the geological and geophysical characteristics of the medium, and a direct relationship was established between attenuation, composition and active processes in the crust and upper mantle of the studied area. According to the estimated intrinsic attenuation (Qi) and scattering attenuation (QSC) contributions into the total attenuation, intrinsic attenuation is generally dominant in the studied area, while the QSC component increases in the areas of large active faults.
abstract_unstemmed	Our detailed study of the crust and upper mantle of the South Baikal basin focused on seismic coda and seismic S-waves attenuation and estimated seismic quality factor (QS and QC), frequency parameter (n), attenuation coefficient (δ), total attenuation (QT), and the ratio of two components the total attenuation: intrinsic attenuation (Qi), and attenuation due to scattering caused by the inhomogeneities of the medium (QSC). We calculated the sizes of inhomogeneities revealed in the block medium, which put their effect on the attenuation of seismic waves in different frequency ranges. The seismic wave attenuation field was analyzed in comparison with the geological and geophysical characteristics of the medium, and a direct relationship was established between attenuation, composition and active processes in the crust and upper mantle of the studied area. According to the estimated intrinsic attenuation (Qi) and scattering attenuation (QSC) contributions into the total attenuation, intrinsic attenuation is generally dominant in the studied area, while the QSC component increases in the areas of large active faults.
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title_short	SPATIAL VARIATIONS OF SEISMIC WAVE ATTENUATION IN THE SOUTH BAIKAL BASIN AND ADJACENT AREAS (BAIKAL RIFT)
url	https://doi.org/10.5800/GT-2019-10-1-0408 https://doaj.org/article/fa718bbe414b44dd905aaec8ea5353fc https://www.gt-crust.ru/jour/article/view/774 https://doaj.org/toc/2078-502X
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author2	P. A. Predein V. A. Sankov Ts. A. Tubanov D. P.-D. Sanzhieva E. A. Gorbunova
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up_date	2024-07-03T22:54:35.887Z
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SPATIAL VARIATIONS OF SEISMIC WAVE ATTENUATION IN THE SOUTH BAIKAL BASIN AND ADJACENT AREAS (BAIKAL RIFT)

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