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うなぎセミナー 10/8

うなぎセミナー 10/8

セミナー等

SEMINARS

更新日:2020.05.07

Updated: 2020.05.07

  • 開催場所:オンライン(Zoom)
  • Place: オンライン(Zoom)
  • 開催日時:2020年10月8日(木) 14時00分~
  • Date and Time: 2020年10月8日(木) 14時00分~

今週のうなぎセミナーについてお知らせいたします。

Here is information of the Unagi-seminar(Oct 8).

************** うなぎセミナーのご案内 (Unagi-seminar) **************

科目:地震学ゼミナールIV B, D / Seminar on Seismology IV B, D(修士・博士)
日時:2020年10月8日(木)14:00~
場所:オンライン(Zoom)

Date and time:Oct 8 (Thursday), 14:00~
Site:Online by Zoom

====

[発表者 (Presenter)]
Hong PENG

[題目 (title)]
Investigating the foreshocks of large earthquakes in Japan main land

[要旨 (Abstract)]
This is a progress of the previous research. The foreshocks of a mainshock are always regarded as random. However, according to the JMA earthquake catalogue of Japan main land from 2004 to 2019 (16 years), we investigate the possible foreshocks of earthquakes with magnitude larger than 3. We find that the mainshock will most likely occur in 2 days and 5 km after the foreshocks, also we calculate the possible probability of the occurrence. This might be helpful for earthquake forecast.

====

今週のうなぎセミナーについてお知らせいたします。

Here is information of the Unagi-seminar(Oct 8).

************** うなぎセミナーのご案内 (Unagi-seminar) **************

科目:地震学ゼミナールIV B, D / Seminar on Seismology IV B, D(修士・博士)
日時:2020年10月8日(木)14:00~
場所:オンライン(Zoom)

Date and time:Oct 8 (Thursday), 14:00~
Site:Online by Zoom

====

[発表者 (Presenter)]
Hong PENG

[題目 (title)]
Investigating the foreshocks of large earthquakes in Japan main land

[要旨 (Abstract)]
This is a progress of the previous research. The foreshocks of a mainshock are always regarded as random. However, according to the JMA earthquake catalogue of Japan main land from 2004 to 2019 (16 years), we investigate the possible foreshocks of earthquakes with magnitude larger than 3. We find that the mainshock will most likely occur in 2 days and 5 km after the foreshocks, also we calculate the possible probability of the occurrence. This might be helpful for earthquake forecast.

====

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© Research Center for Earthquake Hazards.

© Research Center for Earthquake Hazards.