Weak phases production and heat generation controls fault friction during seismic slip

Hadrien Rattez & Manolis Veveakis

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Sep 20, 2019
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Received Date: 9th September 19

The triggering and magnitude of earthquakes is determined by the friction evolution along faults. Experimental results have revealed a drastic decrease of the friction coefficient for velocities close to the maximum seismic one, independently of the material studied. Due to the extreme loading conditions during seismic slip, many competing physical phenomena are occurring (like mineral decomposition, nanoparticle lubrication, melting, among others) that are typically thermal in origin and are changing the nature of the material. 

Here we show that a large set of experimental data for different rocks can be described by such thermally-activated mechanisms, combined with the production of weak phases. By taking under account the energy balance of all processes during fault movement, we present a framework that reconciles the data, and is capable of explaining the frictional behaviour of faults, across the full range of slip velocities (10-9 - 10 m/s). 

The similarity of microstructures observed in nature and in experiments suggests that energetic frameworks like the one presented could quantitatively link observations across the scales and provide deep, physics-based insight on the physical mechanisms driving seismic slip.

Read in full at EarthArXiv.

This is an abstract of a preprint hosted on an independent third party site. It has not been peer reviewed but is currently under consideration at Nature Communications.

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