Dynamic Full‐Field Imaging of Rupture Radiation: Material Contrast Governs Source Mechanism

Abstract

Abstract In seismology, the rupture mechanisms of an earthquake, a glacier stick‐slip and a landslide are not directly observed, but inferred from surface measurements. In contrast, laboratory experiments can illuminate near field effects. The near field reflects the rupture mechanism but is highly attenuated in the case of real‐world surface data. We directly image the elastic wave‐field of a nucleating rupture non‐invasively in its near‐field with ultrasound speckle correlation. Our imaging yields the particle velocity of the full shear wave field at the source location and inside the 3D frictional body. We experimentally show that a strong bimaterial contrast, as encountered in environmental seismology, yields a unidirectional or linear force mechanism for pre‐rupture microslips and decelerating supershear ruptures. A weak contrast, characteristic for earthquakes, generates a double‐couple source mechanism for sub‐Rayleigh ruptures, sometimes preceded by slow deformation at the interface. This deformation is reproduced by the NF of a unidirectional force.

Keywords

• ultrasound imaging for full rupture‐borne shear wave field imaging inside a sliding body
• source mechanism of stick‐slip ruptures on a granular asperity depends on material contrast
• laboratory equivalent to glacier stick‐slip and landslides yields a single force mechanism
• strong bimaterial contrast yields decelerating supershear ruptures
• weak bimaterial contrast yields sub‐Rayleigh rupture propagation
• slow deformation precedes rupture propagation for a weak bimaterial contrast