SEISMICITY AND GPS CONSTRAINTS ON CRUSTAL DEFORMATION IN THE SOUTHERN PART OF THE KOREAN PENINSULA

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dc.contributor.author Jin S.
dc.contributor.author Park P.-H.
dc.contributor.author Li Z.C.
dc.date.accessioned 2025-01-11T06:54:42Z
dc.date.available 2025-01-11T06:54:42Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=14226176
dc.identifier.citation Geosciences Journal, 2006, 10, 4, 491-497
dc.identifier.issn 1226-4806
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/47386
dc.description.abstract Three years of continuous observations at 45 GPS sites in South Korea show horizontal deformation velocities are less than 3 mm/yr with respect to the stable South Korea block. These velocities and the associated horizontal strain rate reveal that South Korea is dominated by both ENE-WSW compression and NNW-SSE extension. Compared to the seismic strain rate in South Korea derived from recently recorded earthquake data (Mw > 4.0, 1936-2004), the principal horizontal axes of both strain rate tensors are nearly consistent, indicating that the seismicity can be used to improve GPS-derived deformation style and orientation. In addition, it also reflects that the occurrence of shallow earthquakes in South Korea is closely related with the horizontal strain.
dc.subject CRUSTAL DEFORMATION
dc.subject GPS
dc.subject KOREAN PENINSULA
dc.subject SEISMICITY
dc.subject STRAIN RATE
dc.title SEISMICITY AND GPS CONSTRAINTS ON CRUSTAL DEFORMATION IN THE SOUTHERN PART OF THE KOREAN PENINSULA
dc.type Статья
dc.identifier.doi 10.1007/BF02910442


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