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AIST On-Site Survey Identifies Surface Fault Associated with the 2005 Pakistan Earthquake.


Tokyo, Japan, Feb 22, 2006 - (JCN JCN Japan Corporate News
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 Newswire) - The National Institute of Advanced Industrial Science and Technology The National Institute of Advanced Industrial Science and Technology (産業技術総合研究所  (AIST AIST Advanced Industrial Science and Technology (Japan)
AIST National Institute of Advanced Industrial Science and Technology (Japan)
AIST Association for Iron & Steel Technology
), in collaboration with Hiroshima Institute of Technology Hiroshima Institute of Technology (広島工業大学  , Tsuru Gakuen, Kyoto University Kyoto University (京都大学 Kyōto daigaku , the Geological Survey of Pakistan Geological Survey of Pakistan (GSP) is located in Quetta, Balochistan, Pakistan. The GSP's mission is to develop, interpret and provide geological information about the country in all its pertinent details that may lead to the prudent management of its natural resources and , and others, conducted an on-site survey of affected area by the magnitude 7.6 earthquake on 8 October 2005 in northern Pakistan Northern Pakistan is the term used to refer to the high-altitude region in the northern part of Pakistan that includes 12 of the world's 27 highest mountains as well as three of the seven longest glaciers outside of the polar regions of the world. . As a result of their work, an outline of the surface fault having a length of approximately 65 km and a maximum vertical displacement In tectonics, vertical displacement is the shifting of land in a vertical direction, resulting in a permanent change in elevation.

Two types of vertical displacement are uplift, an increase in elevation, and subsidence, a decrease in elevation.
 of 5.5m was identified for the first time.

As part of its research on active faults and earthquakes, the AIST conducts urgent surveys of major earthquakes, both in Japan and overseas. Recently, it conducted emergency surveys of the 2004 Sumatra earthquake Sumatra earthquake maty refer to:
  • 2005 Sumatra earthquake
  • March 2007 Sumatra earthquakes
  • September 2007 Sumatra earthquakes
 and tsunami and the 2003 Bam earthquake in Iran. Furthermore, the predecessor of part of AIST, the Geological Survey The term geological survey can be used to describe both the conduct of a survey for geological purposes and an institution holding geological information.

A geological survey
 of Japan, the former Agency of Industrial Science and Technology of the Ministry of International Trade and Industry The Ministry of International Trade and Industry (通商産業省 Tsūsho-sangyō-shō or MITI) was one of the most powerful agencies in the Japanese government.  conducted emergency surveys of the 1999 Izmit earthquake in Turkey and the 1999 Chi-Chi earthquake Ji-Ji earthquake (Traditional Chinese: 集集大地震; Pinyin: jíjí dàdìzhèn  in Taiwan.

On 18-19 January 2006, the Pakistan Geological Survey held the "International Symposium on the 8 October 2005 Pakistan Earthquake: Its Significance and Disaster Mitigation" at Islamabad. Representing AIST were 4 staff members and 2 visiting scholars (one each from Hiroshima Institute of Technology and Kyoto University). Four of the members of the AIST delegation also worked in collaboration with the Geological Survey of Pakistan and Oregon State University Oregon State University, at Corvallis; land-grant and state supported; coeducational; chartered 1858 as Corvallis College, opened 1865. In 1868 it was designated Oregon's land-grant agricultural college and was taken over completely by the state in 1885.  to conduct on-site surveys of the surface fault associated with the earthquake, on 20-22 January and again on 24-28 January, for a total of 8 working days.

To realize a sustainable developed society, AIST has carried out research and development aiming at the minimization of discharge of harmful substances, the enhancement of energy efficiency, and the transformation of raw materials into recycling resources.

For this purpose, AIST and Osaka Organic Chemical Industry have jointly carried out the development of a microreactor which is most suitable for synthesizing medical intermediates, and worked on the synthesis of aldehydes, which are useful as medical intermediates, using the microreactor.

As a result of thesurveys, a 65 km-long fault was confirmed to have appeared on the ground surface (Figure 1) and researchers were able for the first time to get a picture of the entire fault that caused the earthquake.

The main part of the fault, an approximate 50 km-long section running from the NW to the central part of the fault strand, showed major displacement that was dominated by reverse fault components. Their measurements show maximum vertical displacement to be approximately 5.5 m (the NE side-up), and maximum net displacement to be approximately 9 m including a horizontal component. In addition, at several survey sites minor right-lateral slip components were identified. It is also noted that in the main fault section between the NW and central strands, there was discontinuity and bending of the fault line.

Along the SE strand, the continuity of the surface faulting was unclear. Only at two locations in a mountains fault ruptures were found to be occurring with small amount of right-lateral displacement of not more than a few dozen centimeters.

Judging from the distribution of the newly discovered surface fault, it appears that the earthquake occurred when a 20-30 km-long fault segment in each of the NW and central areas ruptured with major displacement. Then, somewhat small-scale displacement in the SW area may also have led to some rupturing.

The main part of the surface fault responsible for the earthquake appeared along an active fault that had previously been known to exist (Nakata et al., 1991; Tanaka and Kumahara, 2005 and 2006). In addition, the distribution and amount of displacement of the identified surface fault roughly corresponded to the those of crustal movements during the earthquake analyzed from satellite observations, as well as to the under-ground rupture process that was analyzed from seismic waves.

Areas where damage was especially severe, such as in the town of Balakot and the northern hamlets of Muzaffarabad, were either just on the surface fault, or very close to it. The rate of house collapse tended to be greater near the fault than in surrounding areas. These findings suggest that ground deformation resulting from fault displacement caused particularly severe damage, and that ground shaking was especially intense near the fault.

About AIST

The National Institute of Advanced Industrial Science and Technology (the new AIST) began operations on April 1, 2001. AIST is a newborn research organization that comprises 15 research institutes previously under the former Agency of Industrial Science and Technology (the former AIST) in the Ministry of International Trade and Industry and the Weights and Measures weights and measures, units and standards for expressing the amount of some quantity, such as length, capacity, or weight; the science of measurement standards and methods is known as metrology.  Training Institute. The new AIST is Japan's largest public research organization with many research facilities and around 3,200 employees in all.

Source: AIST

Contact:
AIST Planning Headquarters
1-3-1, Kasumigaseki, Chiyoda-ku,
Tokyo, 100-8921 Japan
Tel +81-3-5501-0830
Fax +81-3-5501-0855


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Date:Feb 23, 2006
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