Fig. 3.From: Aftershock observation of the 2011 off the Pacific coast of Tohoku Earthquake by using ocean bottom seismometer networkP-wave velocity structure models for the hypocenter determination. The red dotted line and blue dotted line denote the P-wave velocity models for the preliminary location and the double-difference method, respectively. The model is derived from the refraction experiment carried out using the OBSs, an airgun array and explosives in 2008 (Nakahigashi et al., in preparation).Back to article page