Microseismicity of back-arc rifting in the middle Okinawa Trough

Mathematics – Logic

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

4

Earth Crust, Earthquakes, Geological Faults, Geological Surveys, Japan, Ocean Bottom, Pacific Ocean, Seismology, Troughs, Geophysics, Islands, Maps, Seismographs

Scientific paper

A one month microearthquake survey was conducted at Iheya Knolls in the middle Okinawa Trough in 1992 to reveal microearthquake characteristics of back-arc rifting. We deployed five ocean bottom seismometers and observed over 1700 events during 30 days. Hypocenters were determined for 48 earthquakes with good resolution. From this survey, we conclude that the survey area with 100km x 100km has high seismicity, many earthquakes occur in the western part of Iheya Knolls, and few occur in the central part. The earthquakes are distributed in an en echelon shape and throughout the entire depth of the crust. There is no evidence for the existence of transform faults, suggesting that the middle Okinawa Trough is in a stage of back-arc rifting.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Microseismicity of back-arc rifting in the middle Okinawa Trough does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Microseismicity of back-arc rifting in the middle Okinawa Trough, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Microseismicity of back-arc rifting in the middle Okinawa Trough will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-869322

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.