National Earthquake Science Center (NCS) Of One statement In Said Went Is That Thursday To Tibet In 3.3 intensity Of Earthquake Cameред Earthquake 10 kilometers of shallow depth But Came, By which it aftershock Of For susceptible Is. Earlier on November 18, another earthquake of 4.2 magnitude occurred at a depth of 10 kilometers. Earthquakes are generally more dangerous than deep earthquakes. This is because shallow earthquakes produce seismic The waves have a shorter travel distance to the surface, resulting in greater ground shaking and greater damage to structures and more casualties. Possibility it occurs.
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Tibetan Plateau tectonic caused by collision of plates seismic Known for its activities.Tibet And Nepal is a major geological are located on the fault line where the Indian tectonic plate Eurasian Plate collisions, and resulting earthquakes, are a regular occurrence. this area tectonic due to rise seismic It is extremely active and can be powerful enough to change the height of the Himalayan peaks. tibetan plateau indian tectonic plate’s Eurasian caused by collision with plate earth’s crust It attains its height due to the thickness of the Himalayas. faults within the plateau, strike slip And is connected to common systems. The plateau is spread in the east-west direction, which is evidenced by the location in the north-south direction. strike graben, strike slip faulting And GPS data get from.
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In the northern region, strike slip faulting tectonics is the predominant style of, while in the south, the predominant tectonic Area generally situated in north-south direction fault But there is east-west extension. southern Tibet For the first time using satellite images in the late 1970s and early 1980s, seven north-south oriented cracks and normal faults were discovered. Their formation began during a time of expansion about 4 to 8 million years ago.