Item Description
In the hours following the 2011 Honshu event, and as part of tsunami warning procedures at the Laboratoire de Ge ́o- physique in Papeete, Tahiti, the seismic source of the event was analyzed using a number of real-time procedures.
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Media Type
Layer Type
Archive
Seeds
Geolocation
42.058, -87.676
Location(text)
42.0575004, -87.67586210000002
Latitude
42.058
Longitude
-87.676
Location
42.058,-87.676
Media Creator Username
NDL-sensyo
Media Creator Realname
NDL-sensyo
Frequency
Archive Once
Scope
One Page
Language
English
Media Date Create
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English Title
Northwestern University｜From 3-Hz P Waves to 0S2: No Evidence of A Slow Component to the Source of the 2011 Tohoku Earthquake [PDF]
English Description
In the hours following the 2011 Honshu event, and as part of tsunami warning procedures at the Laboratoire de Ge ́o- physique in Papeete, Tahiti, the seismic source of the event was analyzed using a number of real-time procedures.
old_attributes_text
frequency | Once | scope | Page | email | sensyo@ndl.go.jp | language | English|
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URI
http://wayback.archive-it.org/2438/20110301000000/http://www.earth.northwestern.edu/people/emile/PDF/EAO222.pdf
Attribution URI
http://www.earth.northwestern.edu/people/emile/PDF/EAO222.pdf