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Titlebook: British Upper Carboniferous Stratigraphy; C. J. Cleal,B. A. Thomas Book 1996 Springer Science+Business Media Dordrecht 1996 Carboniferous.

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期刊全称British Upper Carboniferous Stratigraphy
影响因子2023C. J. Cleal,B. A. Thomas
视频videohttp://file.papertrans.cn/192/191184/191184.mp4
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图书封面Titlebook: British Upper Carboniferous Stratigraphy;  C. J. Cleal,B. A. Thomas Book 1996 Springer Science+Business Media Dordrecht 1996 Carboniferous.
影响因子This volume summarizes the results of a survey of British Upper Carboniferous sites, undertaken between 1978 and 1990 as part of the Geological Conservation Review (GCR). The GCR was the first attempt to assess the scientific significance of all Britain‘s geological sites and has proved a landmark in the development of a coherent geological conservation strategy in this country. To ensure that the assessments were based on a firm logical and scientific foundation, the range of scientific interest was divided into ninety-seven discrete subject ‘blocks‘, reflecting the natural divisions of stratigraphy, palaeogeography and geological process; Westphalian stratigraphy and Namurian stratigraphy were two of these blocks. The first stage in the survey was a review of the literature, to establish a compre­ hensive database of sites. From this, a provisional list of potentially significant sites was made and this was circulated to all relevant specialists in this country and abroad. At the same time, the sites were visited to assess their physical condition and whether the interest was still extant. In some cases, excavation (so-called ‘site-cleaning‘) was carried out to see if the interes
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Nguyen Phong Nguyen,Emmanuel Mogajinorthern England (the Westphalian D base stratotype has yet to be selected, although sites in South Wales will probably be strong contenders). Because of their importance for stabilizing the definitions of the stages, these stratotypes have a rather different status from the other sites dealt with i
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Nguyen Phong Nguyen,Emmanuel Mogajixtends from Pontypool in the east to near Kidwelly in the west. Carmarthen Bay separates this from a smaller area of outcrop in Pembrokeshire. With the exception of the Iberian Peninsula (Lemos de Sousa and Oliviera; 1983, Martinez Diaz, 1983), South Wales provides by far the best exposed sequences
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Nii Nookwei Tackie,Thomas Anning-Dorsoneas of outcrop, which are known, from west to east, as the Shrewsbury, Coalbrookdale, Wyre Forest, South Staffordshire and Warwickshire coalfields; there are also small areas of outcrop in the Clee Hills of Shropshire (Figure 7.1). The coalfields of North Wales (Denbigh and Flint) and a small outcro
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