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Here, (1) where is the average gravity change rate at the i th station during 2004 2009 (2001–2009 for the reference site A1), N is the total number of observation sites, and σis the standard deviation of the linear regression against the observations at the ith station (solid lines in Figs. 3 and 4, see also column (e) of Table 1).
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Open squares show the F-net stations; solid squares show the JMA stations.
(a) Location of the IWTH25 station (red circle) plotted with other K-NET (solid triangles) and KiK-net stations (solid circles).
Fig. 2. The permanent IMAGE magnetometer stations (open circles) and the temporary stations (solid black) that formed the BEAR network in June July 1998.
A time domain waveform inversion technique (Dreger and Helmberger, 1993; Pasyanos et al., 1996), and three KMA stations (solid inverted triangles in Fig. 3), were used.
Seismic stations (solid squares) used in hypocenter locations and isodepth lines of the upper surface of the Philippine Sea slab at 5-km intervals (solid and broken curves; Miyoshi and Ishibashi, 2004) are shown.
Strong ground motions were recorded at 4 stations (solid triangles in Fig. 1(b)) in the Oshika array, which is located about 120 km to the west-north-west of the epicenter.
These origins of the phases are discussed in Section 4. Fig. 1. (Left) Map showing F-net and KiK-net stations (solid square) and the assumed fault plane (rectangle).
GPS time series data at the stations (solid triangles in Fig. 1) along the coast from northern Miyagi to southern Iwate prefectures are shown in Fig. 2, where the displacements at Oshika, Kesen-numa, Kamaishi, and Miyako are represented by red, purple, blue, and green, respectively.
a Observation station locations (solid triangles) at Tungurahua volcano, Ecuador.
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CEO of Professional Science Editing for Scientists @ prosciediting.com