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	present. Orientations of abundant striations on fault surfaces (slickensides) and other features clearly indicate normal or reverse faulting with little or no strike-slip movement (figure 3). The last of these appears re Add to Reading List Document Date: 2011-05-06 05:33:40 Open Document File Size: 3,73 MB Share Result on Facebook

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present. Orientations of abundant striations on fault surfaces (slickensides) and other features clearly indicate normal or reverse faulting with little or no strike-slip movement (figure 3). The last of these appears reAdd to Reading List