The Paragenesis of Sylvine, Carnallite, Polyhalite, and ]Cieserite in Eskdale Borings Nos
667 The paragenesis of sylvine, carnallite, polyhalite, and ]cieserite in Eskdale borings nos. 3, 4, and 6, north-east Yorkshire. (With Plate XXV.) G. ARMSTRO~O, B.Se., F.G.S., K. C. DUNHAM, D.Sc., S.D., F.G.S., C. 0. HAI~VEY, B.Sc., A.R.C.S., F.R.I.C., P. A. SABINe, Ph.D., A.R.C.S., F.G.S., and W. F. WATERS, B.Sc., F.R.I.C. Geological Survey of Great Britain. [Read March 8, 1951.] INTRODUCTION. HE confirmation of the presence of potassium salts in the Permian T evaporites beneath the Whitby district, first found in the D'Arey Exploration Co.'s Eskdale no. 2 (Aislaby) boring (G. M. Lees and A. H. Taitt, 1945), and the discovery by Imperial Chemical Industries in their Eskdale no. 3 (Sleights), no. 4 (Sneaton), and no. 6 (Upgang) borings that these salts exist in workable quality and quantity, has been recorded in a recent historic paper by Dr. A. Fleck (1950). The successful outcome of this boring campaign may well lead to the outstanding development of the present century in economic mineralogy in Britain. In the course of the exploration the Geological Survey has examined in detail the cores obtained, and every facility has been granted by Imperial Chemical Industries for the removal of specimens from the cores for preservation in the national collection at the Geological Museum. The Petrographical Department of the Geological Survey has, on its side, provided reports on the mineralogy of the cores. The present brief summary of these reports, with some additional chemical, X-ray, and petrographical data, is published by permission of the Director of the Geological Survey and with the approval of Imperial Chemical Industries, Limited.
[Show full text]