The serpentine belt is very continuous to Koumac, then is lost for a score of kilometres, apparently covered by Tertiary sedimentary ... This, while explaining the greater schistosity of the rocks east of the serpentine belt, does not explain the greater ... These quartz-chlorite zones have developed in the crush material of the movement planes of the last big thrusts. ... that we get schists weathering out into masses like logs of wood each 5 to 6 feet long and about 2 feet in diameter. That mayanbsp;...
|Title||:||Proceedings of the Linnean Society of New South Wales|