.... A. Speculations concerning palaeohydraulic controls of terrestrial sedimentation Bull, geol. Soc. Am 1968 79 1573 88 Simpson S. On the trace fossil Chondrites Q. J. geol. Soc. London 1957 112 478 96 Simpson S. The Lynton Beds of North Devon Proc. Ussher Soc 1964 64 14 23...

... the vertical. It is then necessary to correct the “apparent” dip of beds as observed in the core for errors introduced by the deviation of the bore hole from the vertical. Lynton recognized the need for the latter correction, and in his first article on magnetic core orientation 10 described...

... at about 3 °0 in the southern limb of a major anticline with Lynton Beds occupying its core. The axis of the anticline extends WNW from the vicinity of the Brendon Hills of Somerset towards Lynton and out into the Bristol Channel (op. dt., fig. IO). The density measurement of Bott et al. (I958) indicate...

... in 1937 by Laurence I. Durgin, under the direction of Martin Van Couvering. A similar instrument was pictured by Lynton 10 in this Bulletin in the same year. These instruments are valuable when available, because they not only provide a rapid method of solution, but also enable the operator...

... Tunbridge I. P. Whittaker A. Scrutton C. T. North Devon: Lower and Middle Devonian. Lynton Beds and Hangman Sandstone Group International Symposium on the Devonian System. A field guide to selected areas of South-West England 1978 Palaeontological Association 8 13 Van de Kamp P. J...

... mesothrusts 20–44°SSW (some reoriented) WNW–ESE (105°) −35 m–OD 160 m (rs) bed length balance 1.5 km NNE (rs) line length balance Lynton F Moderate SSW WNW–ESE (105°) −300 m–7 km? 2 km NNE (rs) + Devonian component? Post-Carboniferous displacements GMF 40–70°SSW WNW...

...Lynton S. Land Abstract The slipfaces of modern beach dunes on Sapelo Island, Georgia, are deposited by the prevailing competent dry winds rather than the high energy storm winds. High angle cross-bedding (cross-bedding which dips at least 30 degrees ) records the orientation of the prevailing...

...Robert A. Morton; Lynton S. Land In contrast to our acetate-type water, and despite massive rock/water interaction ( Land et al, 1987 ), we cannot account for highly saline Ca-rich water by reactions within the Frio section itself. If our explanation is correct, that Ca-rich water is derived...

...-Triassic Upper Culm tUpper Lower Culm JCarboniferous /Lower Pilton Beds Carboniferous Baggy and ! Marwood Beds ~ Upper Pickwell Down Sandstone t Devonian Morte Slates Ilfracombe Beds Hangman Grits ], Foreland Grits)~ °wer. Lynton Beds -~x)evoman Jurassic: Kimmeridge Clay to Lower Lias Rhaetic Beds Keuper...

... into nearly completely cemented beds. Decimeter-scale domains of curved horizontal concretion elements reflect the influence of adjacent phreatic flow domains, each with their own particular flow paths. Aragonite and high-Mg calcite shells in the sands were the main source of carbon in calcite cement...

...Edward D. Lynton ABSTRACT The writer describes magnetic conditions associated with some typical structural features in California,—an anticline, a syncline, an outstanding magnetic feature in the San Joaquin Valley, a buried fault near Mount Diablo, a part of Ventura County, and Kettleman Hills...

... including Lynton Beds’. The Reverend Richard Hennah (1766–1846) was chaplain to the Plymouth Garrison from 1804 until his death ( Horner 1847 ; Cleevely 1983 , p. 149). He was author of a memoir and research papers on the geology and palaeontology of the Plymouth district, and was a keen fossil...

...Fig. 18. Drifted plant material preserved in estuarine/shallow marine facies of the Hollowbrook Member. ( a , b ) Image and detail of stranded dense raft of drifted plant material preserved on rippled bedding plane of grey sandstone including possible Calamophyton branch, Woody Bay. Scale bar...

.... Perebaskine of Saint Gaudens, France, both of whom worked with him in this region for 6 years, and also A. J. Eardley and E. D. Lynton for criticism and suggestions in the preparation of this paper. © 1948 American Association of Petroleum Geologists. All rights reserved 1948 American Association...

... for July, 1937, were 48,794 barrels daily from 180 wells (see production curve). The upper Pico beds all appear to contain brackish water which may be due to the impervious middle Pico members excluding any upward migration of the more saline waters known to exist in the underlying sands of the Repetto...

... beds for two of three contacts appropriate for study. Secondary pores and cements of quartz, carbonate, and kaolinite do not correlate with proximity to shale beds, but have a preference for sandstones that had relatively high initial porosities and permeabilities. Thus, the flux of formation water...

... where the post-Miocene shelf edge is buried and downslope sediment transport is not blocked. An expanded section of the northernmost profile demonstrates that a layer of sediment has broken and moved to the lower slope ( Figure 6 ). Other sections in this area clearly show contorted beds commonly found...

.... the Pickwell Down Sandstone and the Hangman Grits of north Devon) are likely to be interbedded with marine shales, siltstones and lime- stones (e.g. the Baggy Beds, Upcott Beds, Morte Slates, Ilfracombe Slates and Lynton Beds). The thicknesses of the Devonian in the southern part of the section may be similar...

...Edward D. Lynton ABSTRACT A practical laboratory method of orienting well cores by their magnetic polarity was first developed by the Standard Oil Company of California’s research department early in 1928. The procedure is designed to determine the original orientation in the ground of cores...