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III.—On the Existence of Rich Phosphate of Lime in the London Basin
Published online by Cambridge University Press: 01 May 2009
Extract
The proof which I gave in June, 1891, of the production of “rich phosphate” by enrichment of phosphatic chalk through the influence of the Tertiary deposit called “bief,” enabled us to foresee the existence of similar rich phosphate in the London Basin; since phosphatic chalk, analogous to that which I had described or discovered in Picardy, especially at Hardivilliers and Hallencourt, had been discovered by Mr. Strahan and described by him in an interesting paper “On a Phosphatic Chalk with Belemnitella quadrata.”
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- Copyright © Cambridge University Press 1896
References
page 342 note 1 Bull. Soc. Géol. France, 3e sér., t. xix, p. 867 et seq.Google Scholar
page 342 note 2 Quart. Journ. Geol. Soc., vol. xlvii, p. 356.Google Scholar
page 343 note 1 A specimen of the “rich phosphate” of Taplow was exhibited at the Geologists' Association at the meeting on July 3, 1896, and is now placed in the Museum of Practical Geology.
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