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Researchers find links between secrets and slow earthquakes
The field team (L) Matt Jersteneger, Mark Sterling, Erine Todd, Calum Chamberlain, Ting Wang, Andrea Perez Silva and Jess Allen. Image: Al -Mawarda/Shed light on the flag
Researchers are working to improve earthquakes along the biggest error in New Zealand – Hikurangi starting – where a huge and tuni earthquake can lead to tens of thousands of losses.
Supporting the eastern coast of the Northern Island, the tectonic plate in the Pacific Ocean under the Australian painting.
Under the Hancranji 9.1 earthquake, the National Emergency Management Agency said that tens of thousands of people can die, hundreds of thousands of displacement can be displaced and that the cost of construction damage may lead $ 100 billion.
Researchers from Otugo, Victoria and Diamond are trying, along with GNS, to establish the relationship between earthquake swarms and the possibility of sudden large earthquakes, as strong shakes continued seconds to minutes, causing widespread damage.
Sands of groups of smaller tremors – many are very small so that it could not be felt – while slow earthquakes occurred “silently” for weeks to months without any vibration.
The researchers systematically analyzed whether the seismic swarms and earthquakes associated with earthquakes in the large bending area of Hikuranji, and whether they had provided early indications of large earthquakes.
They developed an index of earthquakes along the integration area, and scientists captured the major earthquakes who have already known, as well as many small seismology with low capacity that are usually without anyone noticing.
The researchers found a link between swarms and slow earthquakes along an area that is subject to Hikurangi, but often with time delay.
Map of an earthquake for the eastern coast of the Northern Island. Photo: Eastern Coast Laboratory/East
The researchers said that understanding the differences in the delay can help determine what prompted the relationship between secrets, slow earthquakes and large earthquakes.
They said that there are 92 spacious slippage earthquakes in the past twenty years, most of which are along the eastern coast of the northern island, at hesitation that suggested stress in some areas while it is likely to accumulate in other regions.
Despite these results, there have been no major earthquakes along the coast since the start of modern records, which makes it difficult to prove a direct link between slow earthquakes and large earthquakes.
The 2016 Kaikōura earthquake has banned Al -Dawla Highway 1. Photo: Tess MCCLure
Ting Wang, a professor of Utago University, said that some studies indicate a 26 percent chance of the earthquake, which is more than 8 in size on the lower north island in the next fifty years, said Ting Wang, Professor of Ottago.
She said: “We are trying to shorten the time frame because we are currently providing data for the next fifty years, but we hope, we hope to expect for the next year.”
Under the earthquake scenario in Nem 9.1, more than 22,000 victims – mostly in a tsunami – can be injured approximately 26,000 others, assuming that 70 percent of people were able to evacuate.
About 400,000 people can be displaced and 30,000 homes were destroyed or damaged by tsunami alone.
It is estimated that there will be about $ 144 billion in damage to the earthquake and tsunami.
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