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air up botellas, are presenting problems which have become more and 1nore difficult in recent years. This is due to two main factors; the first being that the increasingstrainrate is independant of changes in fault strike and dip. It is suggested that strain rate in comparison to throw rate provides a more robust measure of fault activity as it is unaffected by changes in fault geometry. The outcome of this study is that paleoseismic studies on active faults should take into account fault geometry before choosing sites which may have anomalously high or low paleoseismic offsets. Tickets include two shots
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