The secret of a superpower earthquake in Myanmar is revealed: which caused a catastrophic shift

Rescue work and elimination of the consequences of catastrophic earthquake are still ongoing among collapsed and destroyed roads, and geologists are trying to understand what exactly made the earthquake in Myanmar so destructive. In focus. Technology has appeared its Telegram channel.

Subscribe not to miss the latest and most intrusive news from the world of science! It is known that the earthquake occurred along the Saging's fault and became not only supposed, but, according to scientists, also incredibly quickly and far away. According to a seismicist from the Helmgolz Geonuk Center, Frederick Tilmann, all this indicates that the seismic event was a "super -core earthquake".

It should be noted that this type of earthquake is characterized by the fact that the fault is formed faster than the seismic waves created by it can pass through the rock. This leads to the accumulation and strong release of energy. According to Tilmann, an earthquake in Myanmar is essentially equivalent to a "supersonic jet. " The scientist also notes that this may explain why the earthquake shocks were felt more than 1000 kilometers, for example, in the capital of Thailand.

As a rule, supervision events are extremely rare, but they become more frequent during larger earthquakes. Tilmann and the team looked at the magnitude earthquake 7. 7 and found something interesting: the gap that spreads to the south is accelerated to the speed of ~ 5 km/s, which is much faster than the speed of the landslide - the data indicate the presence of super -disruption.

Scientists also found that the total breakdown length of the break was more than 400 kilometers, and a later analysis of the scientist from the Cambridge University showed that the gap could probably be even longer - up to 500 kilometers. According to the US Geological Service, several factors are influenced by the earthquake, and one of them is the depth of its epicenter.

The power of the earthquake of the earthquake decreases with the increase in the distance from the source of the earthquake, and therefore the force of the shocks on the surface from the underground shocks occurring at a depth of about 500 kilometers is much smaller than if the same earthquake occurred at a depth of only 20 kilometers.

The results of the analysis of scientists indicate that the epicenter of the earthquake in Myanmar was incredibly shallow - only about 10 kilometers below the surface. Scientists believe it can explain why the earthquake was so strong and destructive. At the same time, scientists say that we still need to learn about the earthquake in Myanmar, which happened on March 28. Unfortunately, the details of this catastrophic event will appear incredibly slowly.