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The KJedang Range is interpreted as a granite hors!. Its fa ulted boundary with the Kinta Valley has been later cut and offset by many minor wrench fault s with a domi­ nant northwesterl y strike produced by an approximately east-west directed compress ive stress. Other observed lineations are interpreted as conjuga te shear joints and/or latera l shears forming second or third order structures associa ted with the wrench faults and also with possibly major n orthwesterl y striking wrench fa ulting postulated el sewhere in West Malaysia. Quartz dykes have widened original tension joints. Some vertical movement in northwest striking fault planes is evidenced by the contours of the sub-a llu vial valley flo or and the watershed which crosses the northern part of the va lley. 39

Joint patterns and faulting in Kinta, West Malaysia