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The 2000 Mw 6.8 Uglegorsk earthquake and regional plate boundery deformation of Sakhalin from geodetic dataстатья
Статья опубликована в высокорейтинговом журнале
Статья опубликована в журнале из списка Web of Science и/или Scopus- Авторы: Kogan M.G., Bürgmann R., Vasilenko N.F., Scholz C.H., King R.W., Ivashchenko A.I., Frolov D.I., Steblov G.M., Kim Ch U.
- Журнал: Geophysical Research Letters
- Том: 30
- Номер: 3
- Год издания: 2003
- Издательство: American Geophysical Union
- Местоположение издательства: United States
- DOI: 10.1029/2002GL016399
- Аннотация: Interseismic GPS velocities in Sakhalin indicate that the island moves to the west at 3-4 mm/yr with respect to the Eurasian plate, which is about half of the relative Eurasia - North America plate convergence rate. GPS measurements across the central Sakhalin fault system provide evidence of compressive and strike-slip strain accumulation at a rate тЙд3 mm/yr. Coseismic vertical displacements produced by the August 4, 2000 Mw 6.8 Uglegorsk earthquake in Sakhalin were analyzed by constrained nonlinear inversion which provided evidence for a reverse faulting mechanism on an east-dipping fault plane.
- Добавил в систему: Стеблов Григорий Михайлович