Sentence examples for main fault core from inspiring English sources

Red line marks the location of the main fault core between the hanging wall and footwall.

Though the values for the damage zones in this study are variable, m is relatively lower near the main fault core and increases with distance.

The general decrease in sandstone with distance from the main fault core may also contribute to the variations in deformation behavior.

Deformation in the intact zone is more intense near the main fault core, whereas deformation in the surrounding damage zone increases with distance from the fault core.

The surrounding damage zone has the largest total fracture distribution except near the main fault core, where the intact zone has the largest fracture density.

Fracture density in the intact zones generally decreases with distance from the main fault core, indicating that the structures in the intact zones are related to the primary fault activity of the Nobeoka Thrust (Figures 9 and 16).

Brecciation and cataclasis localized only along the main slip surfaces of the oblique normal faults, forming a zone of intense deformation, the fault core, surrounded by less-deformed fractured, faulted and fragmented carbonates of the damage zone.

On the contrary, the transition from the fault core to the hangingwall protolith is sharply defined by the upper main slip surface.

Observing this, my friend gave me an annoyed look, pounded down a shot of whiskey and asked "when was the last time you just dated someone?" In one simple, drunken, straight-to-the-core sentence, my friend not only managed to expose my main fault as a lover, but had also unknowingly exposed me as the standard setting misogynist male that I'd tried my whole life to avoid becoming.

Tracings of microfracture networks of 19 oriented thin sections from a 400 m long transect across the main fault trace was carried out to estimate the hydraulic properties of the low-strain fault damagezone, adjacent to the high-strain fault core, by assuming penny-shaped microfractures of constant radius and aperture within an anisotropic fracture system.

The main orientations of enhanced fracture permeabilities in Cleebourg change from N to S close to the fault core to NE SW in the damage zone.