News Quake in China may have killed scores

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A recent earthquake in Sichuan, China, has reportedly resulted in over 100 casualties, according to local media cited by the state-run China News Service. The earthquake was initially measured at a magnitude of 7.0 by the seismological bureau, while the U.S. Geological Survey recorded it at 6.6. Its shallow depth of approximately 12 kilometers (7.6 miles) contributed to the potential for severe damage. The earthquake is linked to the Longmenshan fault, which was also responsible for the devastating 2008 Sichuan earthquake. The tectonic activity in the region is driven by the convergence of the Indian and Eurasian plates, resulting in significant seismic events over the past decades. Historical data indicates that the area has experienced multiple destructive earthquakes, highlighting its vulnerability to seismic activity.
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Another earthquake.

A state-run China News Service, quoting unnamed local media, said more than 100 people may have been killed or hurt in the earthquake.

The seismological bureau initially measured the quake at magnitude-7, while the U.S. Geological Survey recorded it at 6.6-magnitude, powerful enough to cause severe damage. Its depth was shallow, less than 13 kilometers or 8 miles, which could magnify the impact.

http://www.cbsnews.com/8301-202_162-57580556/quake-in-china-may-have-killed-scores/
 
Physics news on Phys.org
http://earthquake.usgs.gov/earthquakes/eventpage/usb000gcdd#summary

BBC Reports: China earthquake: 'Hundreds dead or injured' in Sichuan
http://www.bbc.co.uk/news/world-22228225

It was at a depth of 12km (7.6 miles), so lots ot energy at the surface.

USGS said:
Tectonic Summary
The April 20, 2013 UTC Mw6.6 earthquake in the Sichuan province of China occurred as the result of east-west oriented reverse-type motion on a north-south striking fault. A preliminary source location suggest the event likely occurred on the Longmenshan fault or a tectonically related fault at a depth of 12km. The Longmenshan fault was the source fault of the May 12, 2008 Mw7.9 Sichuan earthquake. The preliminary April 20 event location is approximately 85km from the hypocentral location of the 2008 Sichuan earthquake. The April 20 earthquake reflects tectonic stresses resulting from the convergence of crustal material slowly moving from the high Tibetan Plateau, to the west, against strong crust underlying the Sichuan Basin and southeastern China.

On a continental scale, the seismicity of central and eastern Asia is a result of northward convergence of the India plate against the Eurasia plate with a velocity of about 50 mm/y. The convergence of the two plates is broadly accommodated by the uplift of the Asian highlands and by the motion of crustal material to the east away from the uplifted Tibetan Plateau.

Four events of Mw6.0 or greater have occurred within 200km of the April 19 event in the past 40 years, including the May 2008 Sichuan earthquake and a subsequent aftershock. The northwestern margin of the Sichuan Basin has previously experienced destructive earthquakes. The magnitude 7.5 earthquake of August 25, 1933, killed more than 9,300 people, while the May 12, 2008 killed 69,197.

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