WebOct 23, 2015 · To date, many researchers have studied 3-D P-wave velocity (Vp) structure of the Japan subduction zone using P-wave arrival-time data from local earthquakes and teleseismic events (see Zhao 2015a, b for comprehensive reviews). These studies have clearly revealed the high-velocity (high-V) subducting Pacific slab and low-velocity (low … WebOct 28, 2024 · We apply a regional tomography method to P-wave travel-times from both local and teleseismic events (Toyokuni et al., 2024a; Zhao et al., 1994, 2012). The joint use of local and teleseismic data can significantly improve the vertical and lateral resolutions of the structure throughout the upper mantle because nearly horizontal rays from local ...
Applied Sciences Free Full-Text Teleseismic Tomography for …
WebThe teleseismic events ( M ≥ 6.0) used are located in a distance range of ~30° to 90° from central Japan ( Fig. 2B ). Many of the local events occurred in the subducting Pacific slab close to the middle portion of the slab (>25-km depth below the slab surface; Fig. 2A ), which can notably improve the tomographic resolution in the Pacific slab. WebAbstract An automatic detection algorithm has been developed which is capable of time P-phase arrivals of both local and teleseismic earthquakes, but rejects noise bursts and … flame breath project slayer
Moho Offset Across the Northern Margin of the Tibetan Plateau
WebAt teleseismic distances (greater than 1000 kilometers) from the epicenter, inelastic effects are unimportant and seiches are generated solely by seismic surface waves. After the … WebMar 27, 2024 · All the teleseismic events are selected according to the following criteria: (1) the magnitudes are greater than 5.5; (2) the epicentral distances fall in the range of 30°∼90°, and (3) each event was recorded at 6 or more stations. WebTeleseismic earthquakes occur at distances greater than 1,000 km from the measurement (seismograph) site. P and S waves are refracted and speed up in faster layers at depth. … canpcs18l