Hexbyte – Tech News – Ars Technica | 2017 earthquake off Mexico broke through an entire tectonic plate

Hexbyte – Tech News – Ars Technica |

Ground Fault Interrupt —

Magnitude 8.2 in Mexico involved more fault movement than thought possible.

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Map of shaking intensity around the epicenter of the September 8, 2017 magnitude 8.2 earthquake.

September 2017 saw a pair of weird earthquakes in Mexico. A magnitude 8.2 on September 8 just offshore the state of Chiapas was followed by a magnitude 7.1 on September 19—this time much closer to Mexico City, causing considerable destruction there. While the two earthquakes were not connected, they were the same type of earthquake, which is unusual in the region.

Mexico’s western coast is a tectonic plate boundary, where the Pacific plate collides with and dives beneath the continent. That means that earthquakes along that boundary are typically the result of compressive force that squeezes rock to slide up the plane of the fault. Both September earthquakes were the result of stretching, however, which is almost as much of a head-scratcher as finding that part of your car’s engine was pulled apart during a head-on crash.

The explanation here is that as the oceanic plate disappears beneath the continent, it sinks downward into the mantle. First of all, the bending of the plate downward causes stretching, just as the skin over your elbow has to stretch. Second, the sinking plate pulls downward as it “hangs” from the part of the plate that is still up at the surface—another stretching force. Occasional earthquakes within this bending, sinking plate can reflect that stretching.

A new study led by the University of Oregon’s Diego Malgar found something even weirder, though. Counter to what we thought possible, the fault seems to have broken clean through the entire tectonic plate.

Hexbyte - Tech News - Ars Technica | The tectonic plate boundary known as a subduction zone, where an oceanic plate dives down beneath another plate.

The tectonic plate boundary known as a subduction zone, where an oceanic plate dives down beneath another plate.


The shaking recorded at seismometers can be used to pinpoint the location of an earthquake, but more detail can be extracted if you have things like GPS sensors in the area detecting ground movement. Seismologists can model the process backward from the measured surface movement and figure out how the fault moved underground. That’s what Malgar and his colleagues did here, producing estimates of the portion of the fault plane that slipped an

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