Abstract
In a previous paper the writer briefly alluded to the evidence, as known from the deep borings in East Kent, afforded by the Palaeozoic and Mesozoic rocks, of the operation of a posthumous axis of unrest, probably of Charnian affinity. This conception receives further support from a study of the special characters exhibited by the Wealden of East Kent and the nature of the unconformity between these strata and the Mesozoic and Palaeozoic rocks underlying them.
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