Detection of precursory slips on a fault by the quiescence and activation of seismicity relative to the ETAS model and by the anomalous trend of the geodetic time series of distances between GPS stations around the fault(B072)(abs.)

Authors=OGATA Yoshihiko

Journal/Book_names=Programme and Abstracts, the Seismological Society of Japan, Fall Meeting

volume=2006

pages=75-75

Publish_year=2006

Publish_Country=JPN

Publisher=Seismological Society of Japan

Language_of_Text=JA

ID=200630143