Garnet crystal microstructures formed during ancient earthquake provide evidence for seismic slip rates along a fault

February 23, 2017 by Bob Yirka report
Focused ion beam image of small mineral inclusions that formed inside the fragmented garnet crystal due to fluid transport into pores in the garnet in the wake of the earthquake. The largest inclusions are about 20 micrometers long. Credit: Made by Oliver Plümper

(Phys.org)—A team of researchers from Norway, France and the Netherlands has found a new way to identify and measure seismic slips that occurred along fault lines during ancient earthquakes. In their paper published in the journal Science Advances, the team describes their study of garnet crystals found along a fault zone and what they discovered.

Because of erosion, there are very few ways to identify or measure an that occurred in the distant past. For that reason, geologists have been looking for better markers. In this new effort, the researchers report on one new marker in Norway that they believe could prove useful for identifying similar early earthquakes in other parts of the world.

To learn more about ancient earthquakes, the researchers were studying rocks along a at Bergen Arcs in western Norway. There, they came across garnet formations that looked as if they had been melted and smeared as the edges of two continents slid past one another. They extracted some samples and took them back to their lab for analysis. Peeking at them through a microscope revealed microfractures so small that they did not change the shape of the rock.

A closer look showed that melted material had been injected into the fractures leaving behind a network of minerals, among them uranium. The team suggests the micro-fracturing occurred as a result of the earthquake. Next, because uranium decays to lead, the researchers measured the lead content in the material within the fractures, and calculated a date for when the earthquake occurred—approximately 420 million years ago. The researchers also found that they could use the garnet to measure the amount of slippage that occurred between layers of rock. Their calculations indicated the earthquake would have measured 6 to 6.5 on the Richter scale, which means it was relatively strong. They note that humans would not have been around to feel it, but animals at the time likely did.

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3D visualization of the structure. Credit: Made by Oliver Plümper

The researchers suggest their method could be used as a marker for finding other ancient earthquake sites and to aid in measuring their slip rates, and thus earthquake magnitude as well.

Field image showing the fault displacement (visible by the offset of the dark layer) associated with an earthquake of an estimated magnitude around 6. This earthquake occurred in Western Norway some 50 kilometers below the Earth’s surface about 420 million years ago. Credit: Bjørn Jamtveit

Completely fragmented garnet crystal (about 1 millimeter in diameter) located at the earthquake slip surface. The upper left part of the crystal was cut off by the earthquake. Credit: Kristina Dunkel

Explore further: Creating earthquake heat maps—temperature spikes leave clues in the rock

More information: Håkon Austrheim et al. Fragmentation of wall rock garnets during deep crustal earthquakes, Science Advances (2017). DOI: 10.1126/sciadv.1602067

Abstract
Fractures and faults riddle the Earth's crust on all scales, and the deformation associated with them is presumed to have had significant effects on its petrological and structural evolution. However, despite the abundance of directly observable earthquake activity, unequivocal evidence for seismic slip rates along ancient faults is rare and usually related to frictional melting and the formation of pseudotachylites. We report novel microstructures from garnet crystals in the immediate vicinity of seismic slip planes that transected lower crustal granulites during intermediate-depth earthquakes in the Bergen Arcs area, western Norway, some 420 million years ago. Seismic loading caused massive dislocation formations and fragmentation of wall rock garnets. Microfracturing and the injection of sulfide melts occurred during an early stage of loading. Subsequent dilation caused pervasive transport of fluids into the garnets along a network of microfractures, dislocations, and subgrain and grain boundaries, leading to the growth of abundant mineral inclusions inside the fragmented garnets. Recrystallization by grain boundary migration closed most of the pores and fractures generated by the seismic event. This wall rock alteration represents the initial stages of an earthquake-triggered metamorphic transformation process that ultimately led to reworking of the lower crust on a regional scale.

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