6.3 The earthquake shook Nepal and China

A 6.3 magnitude earthquake jolted Nepal and China when it occurred in western Shizang at 20:07:19 UTC at a depth of 10.0 km. The earthquake occurred in an uninhabited area known as the Tibetan Plateau, where the nearest epicenter site is 450.3 km away in Saga, Tibet, China.

Earthquakes in the Himalayas are mostly caused by the continental collision of India and Eurasian plates, which converge at a relative rate of 40-50 mm / year. Intrusion into India north under Eurasia generates many earthquakes, thus making this region one of the most dangerous regions on Earth. The surface expression of the plate boundaries is characterized by the slopes of the Solomon Mountain Range between north and south that head in the west, the Burmese India arch in the east and the Himalayan front that heads from east to west in north India.

The boundaries of the Indo-Eurasia plate are diffuse boundaries, which are located in the region near northern India, within the boundaries of the Indus-Zangbo stitching (also called Yarlung-Zangbo) to the north and the main front front to the south. The Indus-Tsangpo Suture Zone sewing area is approximately 200 km north of the Himalayas and is defined by an exposed aviolet chain along the southern rim. The narrow Himalayan front (<200 km) includes many parallel structures between east and west. This region is characterized by the highest rates of earthquakes and the largest earthquakes in the Himalayas, mainly due to movement on payment errors. Examples of large earthquakes in this highly populated region caused by the reverse slip movement include 1934 M8.1 Bihar, 1905 M7.5 Kangra, and 2005 M7.6 Kashmir. The last two have resulted in a high death toll in the Himalayas earthquakes so far, killing more than 100,000 people and leaving millions homeless. The largest recorded Himalaya earthquake occurred automatically on August 15, 1950 in Assam, eastern India. This right M8.6 earthquake, strike slip, was widely felt in a large area of ​​Central Asia, causing extensive damage to villages in the central region.

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