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III.—Evidence suggestive of Charnian Movement in East Kent

Published online by Cambridge University Press:  01 May 2009

Herbert Arthur Baker
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Extract

A Comparative study of the whole of the evidence concerning the Palæozoic floor beneath the South-East of England and the manner in which the various members of the Mesozoics are disposed upon it has led the present writer to conclude that the area, originally defined by Professor P. F. Kendall, over which the effects of the operation of a “posthumous” Charnian axis may be discerned, can be greatly extended, more particularly to the eastward. The evidence, indeed, strongly suggests the presence of a second Charnian axis beneath Suffolk, proceeding thence south-eastward to North France.

Type
Original Articles
Information
Geological Magazine , Volume 4 , Issue 9 , September 1917 , pp. 398 - 403
Copyright
Copyright © Cambridge University Press 1917

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References

page 398 note 1 Kendall, , “Sub-Report on the Concealed Portion of the Coalfield of Yorkshire, Derbyshire, and Nottinghamshire”: Final Report Royal Comm. Coal Supp., pt. ix, 1905Google Scholar.

page 399 note 1 Arber, Newell, Trans. Inst. Min. Eng., vol. xlvii, pt. v, pp. 677–724, 1914Google Scholar.

page 399 note 2 See Table I, p. 402, at end of paper.

page 400 note 1 Kendall, loc. cit.

page 400 note 2 Lamplugh, & Kitchin, , On the Mesozoic Rocks in some of the Coal Explorations in Kent (Mem. Geol. Surv.), 1911Google Scholar. N.B.—It is not proposed to deal fully with this evidence here. The reader is referred to the memoir quoted, pp. 5–56, for abundant details, and to p. 94 for the significant conclusions arrived at by the authors.

page 400 note 3 See Table of Thicknesses (Table II), p. 403, at end of paper.

page 401 note 1 See Table II, p. 403, at end of paper.

page 401 note 2 In point of fact, the inclusion of the Purbecks still further emphasizes the north-easterly thinning of the Oolites.

page 402 note 1 The Gault overlap has been proved in a deep boring at Calais.

page 402 note 2 Estimated.