Scientists simulate Earth’s middle crust to understand earthquakes

Sketch and corresponding photomicrographs illustrating the micromechanical deformation of thin layer of Carbopol (Ultrez 10, 2 wt%). “Carbopol can be described as a two-phase material: in the optical photomicrographs (right), the tightly coiled microgels or ‘grains’ define darker areas; more aqueous viscous material defines the brighter areas. Gel is stationary while a glass plate (black area) is moved, leading to shear localization close to the glass plate boundary. a, Undeformed Carbopol. b, At low shear strain the viscous material starts to connect, forming a ‘weak’ zone. c, Break-up of microgel grains close to the shear zone. Total shear strain γ = 1.” 

Researchers have for the first time been able to measure a material’s resistance to fracturing from various types of tectonic motions in Earth’s middle crust, a discovery that may lead to better understanding of how large earthquakes and slower moving events interact.

The University of Texas Institute for Geophysics (UTIG), research unit of the Jackson School of Geosciences, spearheaded the discovery. The study was published in the September edition of Nature Geoscience.

Scientists conducted the research using Carbopol, a gel-like substance that can simulate the characteristics of rock formations in Earth’s middle crust because it is simultaneously brittle and malleable.

Researchers performed shear tests on the Carbopol, where a portion of the material is pulled one direction and a portion is pulled in the opposite direction. This is similar to what happens to rock formations in the middle crust during earthquakes or slow-slip events, a type of tectonic movement that resembles an earthquake but happens over a much longer period of time.

Previously, nearly all research into such movements of Earth’s crusts was done by measuring tectonic movement using GPS readings and linking these findings with friction laws. Those observations did not address how rock behaves when it softens under heat and pressure.

“It is not really clear how slow-slip events interact with earthquakes, whether they can trigger earthquakes or it’s the other way around — that earthquakes trigger slow-slip events,” said Jacqueline Reber, the study’s lead author who performed this research as postdoctoral fellow at UTIG, and who is now an assistant professor at Iowa State University.

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The research also adds insight into middle crust strain transients, temporary stress on surrounding rock that’s caused by tectonic motion.

“By understanding the mechanics of strain transients a little bit better, we eventually hope to get better insight into how they relate to big, catastrophic earthquakes.”

Unlike slow slips events, earthquakes — or stick-slip events — occur when surfaces quickly alternate between sticking to each other and sliding over each other.

“While earlier studies focused mostly on frictional behavior as an explanation for strain transients we focus in our work on the impact of rheology (how a material flows under stress), especially when it is semi-brittle,” said Reber.

The semi-brittle middle crust can be compared to a candy bar made of nuts and caramel. The nuts represent the brittle rock. The caramel represents the ductile rock.

Researchers exposed Carbopol, in which the ratio between brittle and ductile parts determines how much stress it can take before being permanently deformed or breaking, to forces created by a simple spring-powered shearing apparatus. Lower yield stress induced the Carbonol to imitate hotter, more viscous rock from deeper in Earth’s crust by making it more ductile; at higher yield stress it imitated cooler, more brittle rock.

The tests showed viscous deformation and constant creep movement at lower yield stress and slip-stick behavior at higher yield stress. This highlights the importance of a material’s often complex properties for determining the manner and speed it will respond to stress.

Jacqueline E. Reber, Luc L. Lavier, Nicholas W. Hayman. Experimental demonstration of a semi-brittle origin for crustal strain transients. Nature Geoscience, 2015; 8 (9): 712 DOI: 10.1038/ngeo2496

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Note: The above post is reprinted from materials provided by University of Texas at Austin.