A UConn geologist has joined a  scientific expedition off the southwest coast of Japan to learn more about what  causes earthquakes, knowledge that someday could be used in disaster  management.
Tim Byrne, a geologist and associate professor with the  Center for Integrative Geosciences in the College of Liberal Arts  and Sciences, has joined what he described as a “floating University” on a  Japanese drilling ship poised over the Nankai Trough Seismogenic Zone.
The 20-30 scientists aboard the ship Chikyu  (“Earth” in Japanese) are part of a long-term expedition that will take seismic  images, examine the composition of sediments, collect core samples to study,  position sensors on the ocean floor, and search for faulting zones.
There are thousands of earthquakes every month in Japan, Byrne  notes, many of them minor. The area where he is working has not had a major  quake in more than 60 years, although it is prone to them.
The Nankai Trough is between the  Asian and Philippine Sea plates and is one of the most active earthquake zones  on the planet, according to the Japan Agency for Marine-Earth Science and  Technology, the leading marine-earth science research institute in Japan.
The expedition is part of a worldwide, scientific Integrated  Ocean Drilling Program supported by the U.S. National Science Foundation, Japan, the  European Union, and other participating countries.
The goal is to explore the geology below the ocean floor and  study the processes that ultimately cause violent, unpredictable earthquakes.
“Ultimately our dream is to identify precursors,” says Byrne.  Learning more about the warning signs of an earthquake could lead to earlier  warnings and damage prevention.
Byrne will spend six weeks on the drilling ship off Japan at this  stage of the expedition. In early 2009, he will be a co-chief scientist on  another three-month stage of the work.
After all the shipboard work is done, scientists will be able  to monitor the Nankai Trough from land, collecting  data by cable from instruments planted on the sea floor during the research  cruises.
The Japanese government has invested heavily in earthquake  research and instrumentation, Byrne says. 
  
                              
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| Timothy Byrne, associate professor of marine sciences, will spend six weeks on a Japanese research vessel to learn more about what causes earthquakes. | 
| Photo by Frank Dahlmeyer | 
Byrne will be looking for areas along the plate boundary  where there are seismic gaps – where elastic strain is accumulating, and for  fault surfaces, where two areas of rock slip past each other. 
An earthquake  results from a build-up of elastic strain, and there might be  “micro-earthquakes” preceding it, he says.
The ship has a drilling rig that will lower plastic pipes to  the sea floor, where they will collect samples that can then be analyzed on  board.
 It can take 24 hours to lower a pipe to the sea floor. Scientists work  in 12-hour shifts to analyze what comes up.
“It’s pretty intense,” says Byrne.
Successive stages of the expedition will drill deeper, until  samples are collected 5,000 to 6,000 meters or more beneath the sea floor. Oil  companies, in contrast, dig down to about 3,000 or 4,000 meters.
Byrne was chosen for the expedition because of his expertise  in the geology of Japan,  where he had a fellowship in 1990, and in making field observations in areas  where geology is actively evolving.
Last year he spent a sabbatical leave on a Fulbright grant in  Taiwan,  where he climbed into areas accessible only by foot to map faults in the  southern mountains, another geologically active and earthquake-prone area. 
Hear a podcast about Byrne joining the expedition off Japan.