Alamein Range

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1present. 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

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

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Language: English - Date: 2011-05-06 05:33:40
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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 05:32:46