Tectonic movement in the northeast, Indian plate building stress for future earthquake

Scientists have studied tectonic movement in the Northeast, Indian plate building stress for future earthquakes to understand subsurface stress building.

The researchers used data from 11 large-scale seismic stations in the Lohit Valley and 8 stations in the Siang Window in the Arunachal Himalayas. (Image: Getty)

A team of researchers and seismologists has found that the complex tectonics of the northeastern edge of the Indian plate in the eastern Himalayas and the Indo-Burma mountain range (IBR) could increase pressure on earthquakes in the future. They traced the Great Assam earthquake of 1950 to the interaction between these plates.

Interactions between the two can lead to deeper earthquakes in the IBR and crustal earthquakes in the eastern Himalayas. The northeastern edge of the Indian plate is found in the eastern Himalayas being seismically active to a depth of about 40 km, while earthquakes have been observed in the Indo-Burma Ranges (IBR) up to a depth of about 200 km.

In a study published in the Tectonophysics Journal, researchers suggested that this seismic structure forms complex tectonics that led to the Great Assam Earthquake of 1950. The Great Assam Earthquake was an 8.6-magnitude event and is the largest intracontinental earthquake ever recorded with its epicenter. On the border of India and China near the Mishmi Hills in the Arunachal Himalayas.

It is worth noting that the Eastern Himalayas (EHS) in Arunachal Pradesh and the areas adjacent to Assam are known to be one of the most seismically active regions in the world and are located in the fifth seismic zone in India with potential for major earthquakes in India. future.

Interactions between the two can produce deeper earthquakes. (Photo: Pixabay)

“After the 1950 Great Assam earthquake, the area between Upper Assam and the Mishmi Block did not produce any major earthquakes and is considered a seismic gap zone. An earlier study had suggested a closed area in the Mishmi Intrusion District (MT), the Ministry of Science and Technology said in a statement. Indicates increased pressure for a future earthquake.

Led by Dr Devajit Hazarika of the Wadia Institute of Himalayan Geology, the researchers used data from 11 broadband seismic stations in the Lohit Valley and 8 stations in the Siang Window in Arunachal Himalaya. The researchers studied the general seismic pattern in the EHS and the adjacent Indo-Burma (IBR) scales with a particular focus on earthquakes in the Lohit Valley region.

The study indicates that the IBR is more susceptible to deeper earthquakes and the pressure split is expected to be significantly greater than the pressure variance indicating the influence of complex tectonics.

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