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- W3031991036 abstract "T waves recorded at hydrophone and seismic stations following the Papua New Guinea earthquake of 17 July 1998 and its aftershocks show that a small event at 09:02 GMT featured source properties incompatible with an elastic dislocation of appropriate body-wave magnitude (m b = 4.4). These include an exceptional duration (47 s at the Wake Island hydrophone station WK31), a spectrum rich in high frequencies (7 to 12 Hz), and a generally low spectral amplitude. These characteristics can be explained by the model of an underwater slump, accelerating from a standstill and eventually slowing down. The relocation of the 09:02 event is compatible with its location within an amphitheater inside which shipboard cruises in 1998 and 1999 documented the presence of a 4 ¨C km3 geologically fresh slump. We propose that the slump took place at 09:02 on 17 July 1998, i.e.,13 minutes after the mainshock, and that it generated the locally catastrophic tsunami, whose properties (amplitude and distribution of runup; timing) could not be explained by a dislocation model." @default.
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- W3031991036 date "2003-01-01" @default.
- W3031991036 modified "2023-09-25" @default.
- W3031991036 title "T Waves from the 1998 Papua New Guinea Earthquake and its Aftershocks: Timing the Tsunamigenic Slump" @default.
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- W3031991036 doi "https://doi.org/10.1007/978-3-0348-7995-8_4" @default.
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