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low-angle fault

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low-angle fault [′lō ‚aŋ·gəl ¦fȯlt]
(geology)
A fault that dips at an angle less than 45°.


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Winterer thinks they are low-angle faults in which the upper rocks have separated from and slid over the lower rock layers.
Additional drilling and trenching confirmed both the continuation of shallow mineralization north of the existing resources, as well as a deeper zone, assumed to have been originally one zone, offset 50 meters to the east along a low-angle fault.
The target area is centered over the headwaters of San Vicente Creek, where strongly altered and oxidized diorite is cut by a silicified and mineralized low-angle fault breccia, dipping about 20 degrees SW.
 
 
 
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