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Subduction zone extension faults, combined hazards of major earthquakes Virginia Tech News

Subduction zone extension faults, combined hazards of major earthquakes  Virginia Tech News

 


Normally, the uplift caused by tectonic plates moving underneath, called uplift, from subduction zone earthquakes can reach 1 to 3 metres. This is true of most land-based sites affected by the 1964 earthquake, which hit 9.2 on the Richter scale. However, on Montagu Island, spaced faults created 11 meters of uplift and began draining a coastal lagoon, effectively changing its ecosystem from a marine lagoon to a freshwater marsh.

“The island is kind of stuck in the middle of these faults, so any time these faults rupture, they actually record uplift,” DePaulis said. “It has this exaggerated height, which is not common in earthquakes that only occur in a subduction zone.”

DePaolis and her team examined the effects of an extensional fault rupture on Montagu Island. By analyzing 42 sediment samples, they found stratigraphic evidence of the 1964 earthquake and secondary metamorphism caused by the extensional fault. They noticed a clear change in the sediments from lake silt before the earthquake to rooted soil after the earthquake.

“There are certainly islands that are uplifted by subduction zone earthquakes, but they don't necessarily have faults running through them that cause this exaggerated uplift, so it's a really unique place,” said Dora, an affiliate faculty member at the Center for Global Change and the Fralin Life Sciences Institute. .

The researchers believe that a secondary shift from divergence errors was possible. But this idea has been only theoretical so far because this is the first known landmass to record stratigraphic evidence.

The team members also used diatoms, a type of siliceous microalgae preserved within sediments that are sensitive to changes in salinity, to reconstruct ancient environmental changes that occurred following the 1964 earthquake. They found a clear shift from a hypersaline marine lake environment beyond the reach of the tides, suggesting To the height of the coast.

By comparing core sample results from the 1964 earthquake with samples deeper in coastal strata, the research team discovered sedimentary and diatomaceous evidence for three other cases in which an extensional fault ruptured. This evidence is associated with four of the last eight documented subduction zone earthquakes in the region.

“There is a tremendous amount of displacement on these faults that can create really fast, localized, large tsunamis,” DePaulis said. “So, the local tsunami comes very quickly, and right after that, we will have the tsunami that was created by the subduction zone itself. Suddenly, you have these huge, destructive tsunamis coming quickly one after the other.”

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