摘要：The Tokai region of Japan is known to be a seismic gap area and is expected to be the source region of the anticipated Tokai earthquake with a moment magnitude of over 8.Interplate slow slip occurred from approximately 2001 and subsided in 2005 in the area adjacent to the source region of the expected Tokai earthquake.Eight years later, the Tokai region again revealed signs of a slow slip from early 2013.This is the first evidence based on a dense Global Positioning System network that Tokai long-term slow slips repeatedly occur.Two datasets with different detrending produce similar transient crustal deformation and aseismic slip models, supporting the occurrence of the Tokai slow slip.The center of the current Tokai slow slip is near Lake Hamana, south of the center of the previous Tokai slow slip.The estimated moments, which increase at a roughly constant rate, amount to that of an earthquake with a moment magnitude of 6.6.If the ongoing Tokai slow slip subsides soon, it will suggest that there are at least two different types of slow slip events in the Tokai long-term slow slip area: that is, a large slow slip with a moment magnitude of over 7 with undulating time evolution and a small one with a moment magnitude of around 6.6 with a roughly linear time evolution.Because the Tokai slow slip changes the stress state to one more favorable for the expected Tokai earthquake, intense monitoring is going on.
