The development of secondary porosity and permeability in fractured rock
Systems of faults and joints are observed to span many scales of length and displacement. Spacing and orientation are rarely constant within any area of interest to groundwater engineers. It is suggested that the methods used by engineering surface topographists should be applicable to geological fr...
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Durham University
1981
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.291496 |