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Here we present 3D inversion results of 169 MT (magnetotelluric) sites from the central San Andreas fault in California. Previous extensive 2D inversion and 3D forward modelling of the data set revealed significant along-strike variation of the electrical conductivity structure.
We need more examples of the changes in crustal resistivity associated with earthquakes, but we believe that variations in the electrical state are related actively or passively to the generation of earthquakes.
M6.3 - 38km NNE of Masterton, New Zealand
2014-01-20 02:52:44 UTC
Event Time
2014-01-20 02:52:44 UTC
2014-01-20 15:52:44 UTC+13:00 at epicenter
2014-01-19 20:52:44 UTC-06:00 system time
Location
40.650°S 175.864°E depth=27.4km (17.0mi)
Nearby Cities
38km (24mi) NNE of Masterton, New Zealand
39km (24mi) SSE of Palmerston North, New Zealand
49km (30mi) E of Levin, New Zealand
77km (48mi) ENE of Paraparaumu, New Zealand
115km (71mi) NE of Wellington, New Zealand
The Wairarapa is no stranger to large earthquakes, with two very damaging magnitude 7 quakes in 1942, however, the regions last earthquake above magnitude 6 was in 1961.
2014-01-20 07:15:06.6 41.29 N 19.52 E 2 4.2 ALBANIA
2014-01-20 07:12:40.0 41.41 N 14.43 E 2 4.6 SOUTHERN ITALY
2014-01-20 07:05:05.3 37.22 N 28.78 E 5 2.2 WESTERN TURKEY
2014-01-20 06:31:38.1 41.38 N 19.59 E 7 2.6 ALBANIA
2014-01-20 06:29:51.8 41.31 N 19.43 E 7 2.7 ADRIATIC SEA
2014-01-20 06:26:50.0 41.33 N 19.46 E 8 4.3 ALBANIA
2014-01-20 06:24:05.0 39.81 N 26.19 E 12 1.7 NEAR THE COAST OF WESTERN TURKEY
2014-01-20 06:20:23.0 41.29 N 19.44 E 2 2.8 ADRIATIC SEA
2014-01-20 06:18:18.0 36.51 N 27.55 E 7 1.9 DODECANESE IS.-TURKEY BORDER REG
2014-01-20 06:17:02.7 41.25 N 19.46 E 7 2.6 ADRIATIC SEA
2014-01-20 06:06:42.0 40.55 N 35.02 E 4 2.1 CENTRAL TURKEY
2014-01-20 06:04:43.0 38.46 N 16.27 E 19 2.1 SOUTHERN ITALY
2014-01-20 06:00:15.0 41.39 N 19.48 E 10 4.5 ALBANIA
Relatively strong shaking was also recorded on the Kapiti Coast (e.g. up to 0.2 g in Paraparaumu) whereas accelerations recorded in Wellington city were less than 0.05 g. In comparison, ground motions recorded in Wellington during the recent Cook Strait earthquakes ranged up to 0.26g.