Seismicity study of Arunachal Himalaya

Seismicity study of Arunachal Himalaya reveals low to moderate earthquakes at 2 crustal depths

• A study by the Wadia Institute of Himalayan Geology (WIHG) an autonomous institute of the Department of Science & Technology (DST), Government of India, exploring the elastic properties of rocks and seismicity in this easternmost part of India revealed that the area is generating moderate earthquakes at two different depths.
• The team of scientists installed 11 broadband seismic stations along the Lohit River Valley of Arunachal Himalaya to understand the elastic properties of rocks and seismicity in this easternmost part of India, a study that has been published in the ‘Journal of Asian Earth Sciences’.
• In the present study, the WIHG team used both teleseismic (earthquakes that occur more than 1000 km from the measurement site)and local earthquake data with the help of seismometers having a flat velocity response for the frequency range of 0.004-35 Hz.
• Data were continuously recorded at 20 samples per second, and the Global Positioning System (GPS) receivers were used for time synchronization.
• The study which used teleseismic and local earthquake data procured during January 2007-June 2008 has helped map under-thrusting in this easternmost part of the country and can not only help plan construction but also improve earthquake preparedness in the area.

Latest Findings and its significance

• Low magnitude earthquakes are concentrated at 1-15 km depth, and slightly higher greater than 4.0 magnitude earthquakes are mostly generated from 25-35 km depth. The intermediate-depth is devoid of seismicity and coincides with the zone of fluid/partial melts.
• The Tuting-Tidding Suture Zone (TTSZ) is a major part of the Eastern Himalaya, where the Himalaya takes a sharp southward bend and connects with the Indo-Burma Range.
• This part of the Arunachal Himalaya has gained significant importance in recent times due to the growing need of constructing roads and hydropower projects, making the need for understanding the pattern of seismicity in this region critical.
• The crustal thickness in this area varies from 46.7 km beneath the Brahmaputra Valley to about 55 km in the higher elevations of Arunachal, with a marginal uplift of the contact that defines the boundary between crust and the mantle technically called the Moho discontinuity.
• This, in turn, reveals the under-thrusting mechanism of Indian plate in the Tuting-Tidding Suture Zone.
• Extremely high Poisson’s ratio was also obtained in the higher parts of the Lohit Valley, indicating the presence of fluid or partial melt at crustal depths.
• This detailed assessment of seismicity in this region will be helpful for planning any large-scale construction in this region in the future.