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C <br />C <br /> <br />sse <br />90• <br />ed <br />~ ~ <br />W <br />u <br />z <br />~d <br />r <br />i ad <br />J <br />sd <br />la <br />SURFACM. SUILSIDSNCF: <br />\ I \ I ~~y <br />\~\ +r ~ ~\' I/ <br />~ ~ ~~~~ <br />~~ <br /> <br /> <br /> / OIP <br /> <br /> <br /> l S <br />L " T <br /> ~ . . <br />~ <br /> <br /> ~ I ~~ <br />lo• so• w• ,o• so• so• ~o• eo• oo'• <br />a ANGL[ OF DIP OF S[A-t <br />qte. f.tS Pdtxi d •am inctlnulon on Gmlt ulyes (12). Cotatar U.K. Nuioad Cod <br />tto•nl. <br />that the timefdependent portion is much less than the instantaneous one <br />and ie sometimes so small that without ahigh-precision leveling instru- <br />ment it is difficult to detect. This is best illustrated by the subsidence <br />development curve in Fig. 9.2.6 (12), where the veltit.d axis is subsidence <br />expressed as percentage of total subsidence and the horizontal axis de- <br />notes face lurxlion. The curve indicates maximum wbsidence at P ad a <br /> <br /> <br />i <br /> <br />u <br /> <br />