RAS Earth ScienceФизика Земли Izvestiya, Physics of the Solid Earth

  • ISSN (Print) 0002-3337
  • ISSN (Online) 3034-6452

Features of the Sakhalin Mantle Phase Transition Zone Based on Converted Wave Data

PII
S0002333725020037-1
DOI
10.31857/S0002333725020037
Publication type
Article
Status
Published
Authors
Volume/ Edition
Volume / Issue number 2
Pages
36-42
Abstract
The research presents the phase transition zone boundaries’ topography estimates at the depths of about 410 and 660 km on the basis of data set obtained by Sakhalin island seismic station network using receiver function method. A representative data set consisting of 2500 individual PRFs was analyzed. We revealed a depression in the 660 km boundary in the central and northern parts of the island. The 410 km boundary is significantly elevated in the south Sakhalin, while within the rest of the island it is depressed in comparison to the expected standard depth. It has been suggested that the subsidence of the 410 boundary is connected with the presence of hot lower mantle matter in the phase transition zone in the northern part of the island.
Keywords
зона фазовых переходов мантия PRF зона субдукции Сахалин
Date of publication
18.02.2025
Year of publication
2025
Number of purchasers
0
Views
14

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