Hostname: page-component-78c5997874-mlc7c Total loading time: 0 Render date: 2024-11-15T01:27:18.736Z Has data issue: false hasContentIssue false

Further Studies in Chert. I

Published online by Cambridge University Press:  01 May 2009

Abstract

Dr. F. W. Clarke truly observes in regard to the origin of chert: “No one process can account for all the occurrences of amorphous and cryptocrystalline silica, and each locality must be studied in the light of its own evidence.” (Data of Geochemistry, 1916, p. 544.)

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1929

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

(1) Sargent, H. C.The Lower Carboniferous Chert Formations of Derbyshire”: Geol. Mag., 68, 1921, pp. 265–78.CrossRefGoogle Scholar
(2) Reynolds, S. H. Pres. Address, Brit. Assoc. Adv. Sci. Rep. (Sec. C), Oxford, 1926, pp. 65101.Google Scholar
(3) Sollas, W. J. “The Origin and Formation of Flints”: The Age of the Earth, London, 1905, pp. 133–65.Google Scholar
(4) Murray, and Irvine, On Silica and the Siliceous Remains of Organisms in Modern Seas”: Proc. Roy. Soc. Edin., 18, 1891, p. 231.Google Scholar
(5)The Country around Pembroke and Tenby”: Mem. Geol. Surv., 1921.Google Scholar
(6) Tarr, W. A.The Origin of Chert and Flint”: Univ. Miss. Studies, 1, 1926, pp. 144.Google Scholar
(7) Lawson, A. C.Sketch of the Geology of the San Francisco Peninsula”: U.S.G.S. 15th Annual Report, 1895.Google Scholar
(8) Scott, A.Application of Colloid Chemistry to Mineralogy and Petrology”: 4th Report on Colloid Chemistry (Brit. Assoc. Adv. Sci.), 1922, pp. 204–43.Google Scholar
(9) Hallimond, A. F.Bedded Iron Ores of England and Wales”: Special Reports on the Minerel Resources of Great Britain, 29, 1925 (Mem. Gent. Surv.).Google Scholar
(10) Hudson, R. G.On the Rhythmic Succession of the Yoredale Series in Wensleydale”: Proc. Yorks. Geol. Soc., 20, 1924, pp. 125–35.CrossRefGoogle Scholar
(11) Cox, , Dean, and Gottschalk, Studies on the Origin of Missouri Cherts and Zinc Ores”: Chem. News, 115, 1917, pp. 52–4, 65–8, 76–8.Google Scholar
(12) Sargent, H. C.The Massive Chert Formation of North Flintshire”: Geol. Mag., 60, 1923, pp. 168–83.CrossRefGoogle Scholar
(13) Arnold-Bemrose, H. H.The Toadstones of Derbyshire, their Field-Relations and Petrography”: Quart. Journ. Geol. Soc., 63, 1907, pp. 241–81.CrossRefGoogle Scholar
(14) Elles, G. L.The Relations of the Ordovician and Silurian Rocks of Conway (North Wales)”: Quart. Journ. Geol. Soc., 65, 1909, pp. 169–92.CrossRefGoogle Scholar
(15) Bassett, H.Colloid Problems in Analytical Chemistry”: 4th Report on Colloid Chemistry (Brit. Assoc. Adv. Sci.), 1922, pp. 523.Google Scholar
(16) Edward., SampsonThe Ferruginous Chert Formation of Notre Dame Bay, Newfoundland”: Journ. Geol., 26, 1923, pp. 571–98.Google Scholar
(17) Finlayson, A. M.Problems of Ore-Deposition in the Lead and Zinc Veins of Great Britain”: Quart. Journ. Geol. Soc., 66, 1910, pp. 299327.CrossRefGoogle Scholar