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Read, W. 1994, High-frequency, glacial-eustatic sequences in early Namurian coal-bearing fluviodeltaic . 1994, High-frequency, glacial-eustatic sequences in early Namurian coal-bearing fluviodeltaic deposits, central Scotland, in De Boer, P. and Smith, D. ed. Orbital forcing and cyclic sequences: IAS Special Publications No. 19, p. 413–428. Read, W. and Forsyth, I. 1989, Allocycles and autocycles in the Upper part of the Limestone Coal Group (Pendleian, E1) in the Glasgow-Stirling Region of the Midland Valley of Scotland: Geol. Wagner, R. and Fisher,M.
The upper part of the Limestone Coal Group (Pendleian E1), between the major marine transgressions of the Black Metals and the Index Limestone, represents an early example of ‘coal measures’ facies. It comprises a distal and a proximal facies association. The distal facies association, which was subject to relatively strong marine influences and included both deltaic and fluvial elements, is characterized by a regular ‘layer-cake’ succession with lithological members.
The Limestone Coal Group varies greatly in its development from a thin sandy sequence about 30 m thick with thin coals in parts of Ayrshire, up to 550m in the northern part of the Central Coalfield.
The Limestone Coal Group varies greatly in its development from a thin sandy sequence about 30 m thick with thin coals in parts of Ayrshire, up to 550m in the northern part of the Central Coalfield, where there are about fifteen workable coal seams (P915532). A large part of the Scottish coal-mining industry has been, and continues to be, based on the coals of the Limestone Coal Group.
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December 15, 2009 History. Geological Survey of Great Britain. The limestone coal group of the Glasgow district. 1 2 3 4 5. Want to Read. Wartime pamphlet, Geological Survey of Great Britain - n. 4, Wartime pamphlet - n. 4.
The Upper Limestone Group and Passage Group of Douglas, Lanarkshire. Shoreward facies changes and their relation to cyclical sedimentation in part of the Namurian east of Stirling, Scotland. A. & Dean, . On a boring to prove the Limestone Coal Group near Hamilton, Lanarkshire. for 1936, Part 2, 63–73. Experiments on ripple lamination. A quantitative study of coal-bearing cycles in the Namurian of Central Scotland, 1, Sedimentology, 9, 137–156. & Johnson, S. R. H. 1967.
The Coal Measures is a term for the coal-bearing part of the Upper Carboniferous System. The Coal Measures Group consists of the Upper Coal Measures Formation, the Middle Coal Measures Formation and the Lower Coal Measures Formation. The group records the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks (claystones, shales, siltstones, sandstones, conglomerates) interstratified with the beds of coal. In most places, the Coal Measures are underlain by coarser clastic sequences known as Millstone Grit, of Namurian age.
This article is intended to show a timeline of the history of Glasgow, Scotland, up to the present day. 543: The 12th century Bishop Jocelyn will later claim Glasgow's monastic church was founded by Saint Kentigern, also known as Saint Mungo, i. . 543: The 12th century Bishop Jocelyn will later claim Glasgow's monastic church was founded by Saint Kentigern, also known as Saint Mungo, in this year; he also claimed that Kentigern found at Glasgow a cemetery which Saint Ninian had hallowed. 560: Jocelyn claims Mungo/Kentigern made his first bishop in this year.