2016
DOI: 10.1016/j.rgg.2016.10.007
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Deep seismic structure of the boundary zone between the Eurasian and Okhotsk plates in eastern Russia (along the 3DV deep seismic sounding profile)

Abstract: Analysis of geological and geophysical data on the boundary zones between the Eurasian plate and other plates shows poor knowledge of the deep structure of the region. This information will help to refine the position of the plate boundaries and the structure of the Earth’s crust and mantle. We present data on the seismicity and deep structure along the deep seismic sounding (DSS) profile running across the boundary between the Eurasian and Okhotsk plates. A comprehensive analysis of the DSS materials and seis… Show more

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Cited by 7 publications
(3 citation statements)
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“…e stirrups are also changed from circular spiral stirrups to rectangular closed stirrups to increase large concrete core area [12]. Relevant studies have proved: (1) e main mode of horizontal deformation of hybrid fabricated shear wall is the opening of the gap at the joint, and the shear wall can basically be regarded as a rigid body around the joint.…”
Section: Prestressed Fabricated Building Structurementioning
confidence: 99%
“…e stirrups are also changed from circular spiral stirrups to rectangular closed stirrups to increase large concrete core area [12]. Relevant studies have proved: (1) e main mode of horizontal deformation of hybrid fabricated shear wall is the opening of the gap at the joint, and the shear wall can basically be regarded as a rigid body around the joint.…”
Section: Prestressed Fabricated Building Structurementioning
confidence: 99%
“…A zone of anomalous seismicity and deep structure extends along the DSS profile for several hundred kilometers. It was refined the position of the main boundary between the Eurasian and Okhotsk plates, which passes approximately along 144° E [Solov'ev et al, 2016].…”
Section: Fig 4 Main Russian Vertical Reference Frame (Mrvrf)mentioning
confidence: 99%
“…скорости на поверхности мантии, полученной ме-тодом ГСЗ в 70-80-х годах прошлого столетия для территории Байкальской рифтовой зоны, юга Си-бирской платформы и разновозрастных складча-тых областей Прибайкалья и Забайкалья [Puzyrev, 1981[Puzyrev, , 1993Mishen'kin et al, 1999;Seleznev et al, 2003;Suvorov et al, 2002], и данных профиля 1-СБ 2014-2015 гг. [Solov'ev et al, 2016;Soloviev et al, 2017].…”
Section: площадные сейсмологические исследования по изучению скоростиunclassified