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Subject:
From:
david west <[log in to unmask]>
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Date:
Mon, 12 Jun 2000 08:37:34 +1000
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The progressive surficial delamination of argillaceous sedimentary dimension
stone is attributable to the cumulative combined physicochemical effect of
cyclic hydration, differential thermal expansion and ion exchange in the
clay minerals.

Hope this helps you ][<en!

Cheers

david

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