, Mw = 7.7, Peru earthquake is determined using broadband teleseismic waveforms, a differential SAR interferogram (interferometric synthetic aperture radar [InSAR]), and a fault parametrization allowing slip and rupture velocity to vary along the rupture plane. Both data sets are inverted jointly to limit the trade-off between the space and...
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2003 (v1)Journal articleUploaded on: December 4, 2022
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2004 (v1)Journal article
Bulletin of the Seismological Society of America, v. 94, n. 6, p. 2015-2027, 2004. http://dx.doi.org/10.1785/0120030038
Uploaded on: December 4, 2022 -
2002 (v1)Journal article
Bulletin of the Seismological Society of America, v. 92, n. 1, p. 278-299, 2002. http://dx.doi.org/10.1785/0120000806
Uploaded on: December 4, 2022 -
September 15, 2016 (v1)Journal article
Magma movement or reservoir pressurisation can drive swarms of low-magnitude volcano-tectonic earthquakes, as well as occasional larger earthquakes (>M5) on local tectonic faults. Earthquakes >M5 near volcanoes are challenging to interpret in terms of evolving volcanic hazard, but are often associated with eruptions, and in some cases enhance...
Uploaded on: February 28, 2023