SOUTH MOUNTAIN
ANTICLINE
This locality in eastern US became synonymous with strain determination
based on deformed oolites that E Cloos carried out in forties, and
eventually published in 1947. The deformed oolites of South Mountain
Anticline were used by Cloos to determine the finite strain and this work
is the first towards the quantitative aspect of finite strain
determination. On the basis of his study, Cloos showed that the strains
were small on the normal but large on the overturned limb of the
anticlinal fold and the long axes of oolites corresponded with the
cleavage trajectories of the fold. However, Cloos was a little perplexed
as the margins of deformed oolites were "frayed" which made
actual micrometric analysis a difficult task. This was because of
extensive pressure solution that gave rise to tectonic stylolites or
spaced PS stripes. He found it hard to excatly measure the long and short
axes of deformed oolites. The actual plastic deformation component of
oolites is rather small. Shankar Mitra in 1978 did work on this antcline
and was able to separate the components of pressure solution from plastic
deformation from deformed rutile crystals in quartz grain |