Relevant bibliographies by topics / Geology - Great Britain - Worksop

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters

Academic literature on the topic 'Geology - Great Britain - Worksop'

Author: Grafiati
Published: 4 June 2021
Last updated: 11 February 2022

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Journal articles on the topic "Geology - Great Britain - Worksop"

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Leveridge, B. E., and R. K. Shail. "The marine Devonian stratigraphy of Great Britain." Proceedings of the Geologists' Association 122, no. 4 (2011): 540–67. http://dx.doi.org/10.1016/j.pgeola.2011.03.003.

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Selley, Richard C. "Petroleum seepages and impregnations in Great Britain." Marine and Petroleum Geology 9, no. 3 (1992): 226–44. http://dx.doi.org/10.1016/0264-8172(92)90072-m.

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McMillan, A. A. "A provisional Quaternary and Neogene lithostratigraphical framework for Great Britain." Netherlands Journal of Geosciences 84, no. 2 (2005): 87–107. http://dx.doi.org/10.1017/s0016774600022988.

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AbstractThis paper presents an overview of a provisional lithostratigraphical framework for the Quaternary and Neogene deposits of Great Britain (England, Scotland and Wales) (onshore). The objective is to provide a workable framework to aid future Quaternary mapping and research, and a stratigraphical scheme capable of use in a wide variety of applications. Using the full hierarchy, a supergroup, group and subgroup lithostratigraphy, based upon the primary mapping unit, the formation, is proposed. It is recommended that some classes of lithogenetically-defined deposits which, at present cannot be accorded formational status, should be assigned informally to one of the proposed groups or subgroups. The framework distinguishes one superficial deposits supergroup within which seven groups are defined: i) Crag Group, marine deposits (Late Pliocene to Early Pleistocene); ii), Dunwich Group, fluvial deposits (pre-Anglian/pre-Elsterian); iii) Residual Deposits Group; iv) British Coastal Deposits Group, coastal and marine deposits (Anglian to Holocene); v) Britannia Catchments Group, fluvial, organic and mass movement deposits (Anglian to Holocene) within broadly defined catchment areas related to Late Devensian to present-day physiography; vi) Albion Glacigenic Group, glacigenic deposits (pre-Devensian/pre-Weichselian), and vii) Caledonia Glacigenic Group, glacigenic deposits (Devensian/Weichselian). North of the Devensian (Weichselian) ice-sheet limit, a series of glacigenic subgroups are defined geographically for the two glacigenic groups on the basis of mappable formations of till. The subgroups include associated formations of glaciofluvial and glaciolacustrine deposits. Consequently some of the glacigenic water-lain units may extend beyond the Devensian limit. Catchment subgroups of the Britannia Catchments Group are proposed for formations and lithogenetic units defined within broad present-day physiographic regions by major river drainage systems that have developed since Middle Pleistocene time. Lithostratigraphical description and correlation of formations will aid the refinement of the proposed framework and enable the development of lithostratigraphical maps and three-dimensional models. As well as offering a unified framework for onshore Quaternary and Neogene deposits the proposed supergroup, group and subgroup structure may prove useful for a wide range of regional applications (e.g. hydrological, hydrogeological, engineering).
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Waldron, John W. F., David I. Schofield, S. Andrew Dufrane, et al. "Ganderia–Laurentia collision in the Caledonides of Great Britain and Ireland." Journal of the Geological Society 171, no. 4 (2014): 555–69. http://dx.doi.org/10.1144/jgs2013-131.

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Ladd, Cai J. T. "Review on processes and management of saltmarshes across Great Britain." Proceedings of the Geologists' Association 132, no. 3 (2021): 269–83. http://dx.doi.org/10.1016/j.pgeola.2021.02.005.

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Mathers, S. J., R. L. Terrington, C. N. Waters, and A. G. Leslie. "GB 3D – a framework for the bedrock geology of Great Britain." Geoscience Data Journal 1, no. 1 (2014): 30–42. http://dx.doi.org/10.1002/gdj3.9.

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Orlowski, Stanislaw. "Cambrian stratigraphy and stage subdivision in the Holy Cross Mountains, Poland." Geological Magazine 129, no. 4 (1992): 471–74. http://dx.doi.org/10.1017/s0016756800019555.

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AbstractThe lithostratigraphic and biostratigraphic subdivisions of the Cambrian sequence in the Holy Cross Mountains of Poland are briefly presented and discussed. In accordance with recent progress in Cambrian stratigraphy and correlation in Great Britain and Scandinavia, a new proposal for chronostratigraphic stages is made. It is suggested that these stages are suitable for the Cambrian areas of central and northwest Europe, comprising Great Britain, Scandinavia and Poland. The formal establishment of the stages, a task for the Commission on Cambrian Stratigraphy, could be made using British or Scandinavian stratotypes.
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Baily, H. E., B. W. Glover, S. Holloway, and S. R. Young. "Controls of coalbed methane prospectivity in Great Britain." Geological Society, London, Special Publications 82, no. 1 (1995): 251–65. http://dx.doi.org/10.1144/gsl.sp.1995.082.01.17.

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Bailey, M. T., C. J. Gandy, I. A. Watson, L. M. Wyatt, and A. P. Jarvis. "Heat recovery potential of mine water treatment systems in Great Britain." International Journal of Coal Geology 164 (July 2016): 77–84. http://dx.doi.org/10.1016/j.coal.2016.03.007.

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Parnell, John, Adrian J. Boyce, Brett Davidheiser-Kroll, Connor Brolly, Stephen Bowden, and Paula Lindgren. "Enhanced microbial activity in carbon-rich pillow lavas, Ordovician, Great Britain and Ireland." Geology 43, no. 9 (2015): 827–30. http://dx.doi.org/10.1130/g36937.1.

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Dissertations / Theses on the topic "Geology - Great Britain - Worksop"

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Wilson, Oneta M. "The natural zeolites of Great Britain." Thesis, University of Salford, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239998.

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Preston, Catherine Emma. "Geology, visualisation and the 1893 Hauliers' Strike : an interdisciplinary exploration." Thesis, Cardiff University, 2010. http://orca.cf.ac.uk/54118/.

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The overarching purpose of the thesis is to explore the interaction between the geological structure of the South Wales coalfield and the development of nineteenth century coalfield society. Through a detailed study of a single event, the 1893 Hauliers' Strike, and the use of modern 3D mapping and visualization techniques, the thesis aims to explore how the geology and landscape of South Wales influenced not just the geographical extent and nature o f the coal industry but also the experiences and responses of the human society which grew up around that industry. Although Welsh historians have been aware of the implications of the coalfield's geology for the economic conditions under which the industry operated they have paid less detailed attention to its implications for unity and co-operation amongst the workforce. The emergence of modern mapping techniques, more specifically Geographic Information Systems (GIS), allows testing for the presence of divisive geological influences on human action at a particular point in time. This thesis argues that the strike of 1893 and indeed the history of the coalfield generally cannot be fully understood unless geology is considered. It also argues that GIS offers a powerful way of reimagining past events and landscapes which enhance the historical research process. The thesis is divided into two parts. The first considers the challenges and potential benefits for historical research of the adoption of geological insights and GIS visualisation techniques. The second section will provide a detailed study of the 1893 Hauliers' Strike. Chapters in this section include: an overview of the strike and its historiography; an exploration of the traditional explanations of the strike; evidence for geology as a divisive force acting on the workers' behaviour; and the role of the landscape in the promotion and maintenance of the strike.
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Bessa, Julian L. "High-resolution outcrop gamma-ray spectrometry of the Lower Lias, Southern Britain." Thesis, University of Oxford, 1995. http://ora.ox.ac.uk/objects/uuid:901bed7b-e4e5-4791-8cf1-496430f7f9b1.

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A detailed stratigraphic analysis of the Lower Lias of southern Britain using the technique of gamma-ray spectrometry is presented. Gamma-ray data were collected, at the maximum stratigraphic resolution possible, from the Rhaetian to Pliensbachian successions exposed in southern Britain in the Bristol Channel Basin, Wessex Basin and East Midland Shelf. The data, in the form of measured gamma-ray signatures and hence geochemical profiles, is placed within a biostratigraphic framework. The outcrop gamma-ray logs collected from the Somerset coast (Rhaetian - Lower Sinemurian) can be subdivided, on the basis of both total gamma-ray signature and elemental log-signature into 9 gamma-ray units. These units are at a higher level of resolution than the single LL 1 gamma-ray unit defined by Whittaker et al (1985) for the Blue Lias in the subsurface. Outcrop gamma-ray correlation is possible between Somerset and Glamorgan, in some cases at a resolution greater than that offered by ammonite subzonal biostratigraphy. This resolution of correlation suggests the presence of a stratigraphic gap in Somerset within the johnstoni Subzone of the planorbis Zone. The outcrop gamma-ray logs collected from the Dorset coast (Rhaetian - Pliensbachian) can be divided into 10 gamma-ray units. These gamma-ray units can be correlated with the subsurface succession in the Winterborne Kingston and the Burton Row boreholes. The ability to correlate across numerous fault blocks and between different basins suggests that the controls upon gamma-ray signature were probably regional. A model is presented in which the degree of detrital influence within a fine grained mud and pelagic carbonate depositional system can be qualitatively assessed. Proximal and distal mudrock facies can be identified from the Th concentration log with proximal facies characterised by a Th concentration 10 ppm and above and distal facies characterised by a Th concentration of 8 ppm and below. The Th concentration log can also be used to determine intervals of mudrock progradation (increasing Th concentration) and retrogradation (decreasing Th concentration). These signatures can be interpreted within a sequence stratigraphic framework, of which the genetic stratigraphic model of Galloway (1989) is most applicable to the Lower Lias of southern Britain. The succession can be divided into eight genetic stratigraphic sequences. Maximum flooding surfaces are inferred at condensed limestone horizons of low Th concentration. The distal expression of the sequence boundary (the correlative conformity) is inferred at horizons of highest Th concentration. The development of anoxia within the epeiric sea can only partly be explained in terms of sequence stratigraphy with anoxia developing during periods of relative sea-level fall and rise or not at all.
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Menpes, Robert. "Tertiary uplift and its implications for the tectonic evolution of sedimentary basins, offshore south-west United Kingdom /." Title page, contents and abstract only, 1997. http://web4.library.adelaide.edu.au/theses/09PH/09phm547.pdf.

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Pearthree, Philip Arnim. "Geomorphic analyses of young faulting and fault behavior in central Nevada." Diss., The University of Arizona, 1990. http://hdl.handle.net/10150/185339.

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This dissertation research assesses the behavior of young faults in central Nevada through analyses of landforms associated with these faults. Four large earthquakes have occurred since 1915 in a striking N-S belt in central Nevada; no comparable earthquakes have occurred elsewhere in the Great Basin. The frequency of large-earthquake occurrence, and temporal and spatial patterns and rates of faulting in central Nevada during the Holocene were assessed through geomorphic and geologic studies of young fault scarps. Ages of paleoseismic events were estimated primarily through analyses of fault scarp morphologies and characterization and quantification of soil development associated with alluvial surfaces. Rates of fault scarp degradation were explored through diffusion-based modeling of latest Pleistocene pluvial shoreline scarps. Morphologic scarp age depends strongly on scarp size; modest variations in local climate, particle size, and aspect are less important. Incorporating a factor that depends on scarp size almost always decreases the scatter in scarp age estimates, and is critical if only small scarps exist along a fault zone. An average of ±30% uncertainty about the mean scarp age estimate remains after these analyses. Soil development indices were calibrated using 14 Holocene to latest Pleistocene soil profiles in central Nevada whose maximum ages are constrained. Soil development indices were used to estimate ages of faulted and unfaulted alluvial surfaces along fault scarps. Soils and morphologic fault scarp age estimates for paleoseismic events are generally consistent. Temporal and spatial patterns and rates of faulting during the Holocene were evaluated using age estimates for paleoseismic events. The long-term rate of faulting is about 10 times lower than the historical rate. There were no other N-S belts of faulting during the Holocene, although scarp ages suggest that there may have been other temporal clusters of faulting. There have been spatial clusters of faulting during portions of the Holocene. The extensional deformation rate across central Nevada during the Holocene is about 0.5-0.75 mm/yr. Integrating this rate with fault-slip data from other portions of the northern Great Basin, the Holocene extensional deformation rate is 3.5-6.5 mm/yr, substantially lower than the historical deformation rate.
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Kennedy, Jonathan David. "Palaeoecology, palaeoceanography, mineralogy, and stable isotopes of forminifera and ostracods from the Middle and Upper Jurassic of Great Britain." Thesis, University of Oxford, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.358717.

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Hibbert, Fiona Danielle. "Dynamics of the British Ice Sheet and prevailing hydrographic conditions for the last 175,000 years : an investigation of marine sediment core MD04-2822 from the Rockall Trough." Thesis, University of St Andrews, 2011. http://hdl.handle.net/10023/3136.

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This study presents a stratigraphic investigation of the marine sediment core MD04-2822 from the Rockall Trough (56° 50.54' N, 11° 22.96' W; 2344 m water depth). This core is currently the only available high resolution record for the calibration of Late Quaternary sedimentary sequences of the British (Hebridean) margin. It therefore offers an unprecedented archive of changing sedimentological and climatological conditions for the last 175,000 years. The high resolution, multi-proxy records have enabled surface and deep water conditions within the Rockall Trough to be reconstructed. In addition, the fluctuating nature of ice-rafted debris (IRD) inputs to the MD04-2822 site allows a first order attempt of BIS dynamics for the entirety of the last glacial period (i.e. from the demise of the last interglacial to the decay of the Devensian/Weichselian ice sheet) as well as the majority of the penultimate (Saalian/MIS 6) glaciation. Sediment core MD04-2822 is ideally located to capture the dynamics of the British Ice Sheet (BIS) via a continuous record of IRD and fine-grained terrigenous inputs. Fundamental to this is the construction of a robust chronology. This was achieved via: the correlation of the benthic δ¹⁸O record to a global δ¹⁸O stack (SPECMAP); the correlation of the surface proxies (% N. pachyderma (sinistral) and XRF Ca) to the Greenland δ¹⁸O and Antarctic methane ice core records; and radiocarbon dating. This chronology was validated using both radiocarbon dating and tephra horizons. An evaluation of the event stratigraphy approach used in the construction of the MD04-2822 chronology is presented. The marine record provides a valuable archive of past ice sheet dynamics as much terrestrial evidence is removed or obscured by subsequent ice sheet oscillations MD04-2822 provides the first evidence for the expansion of the BIS onto the Hebridean Margin during MIS6 (thereby confirming previous long-range seismic correlations). The continuous sedimentation at MD04-2822 enabled the first insights into the early dynamics of the last BIS. Increases in IRD and fine grained terrigenous material delivered to the MD04-2822 at ca. 72 kyr represent the first significant delivery of material from the BIS across the continental shelf to the core site. The BIS would therefore have attained a marine calving margin by this time. A multi-proxy investigation of provenance was undertaken, however unequivocal provenance determinations remain problematic. The location of the core suggest the proximal BIS as the most likely source of terrigenous inputs. The expanded nature of the MD04-2822 sediments during the penultimate deglacial (Termination II) provides the first details of BIS dynamics for this period: the interplay of large inputs of freshwater from the decay of the Saalian (MIS 6) ice sheets (including the BIS) upon the surface and deep water circulation of the North Atlantic is investigated. In addition, sub-orbital climatic variability is documented at this location throughout the last interglacial (MIS 5e) and appears to be an intrinsic feature of both the N.E. Atlantic surface and deep water circulation of the last 175 kyr.
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Books on the topic "Geology - Great Britain - Worksop"

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1947-, Harris Charles, ed. The periglaciation of Great Britain. Cambridge University Press, 1994.

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Geology and environment in Britain and Ireland. UCL Press, 1994.

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Geology of the Peterborough district. H.M.S.O., 1989.

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A, Thomas Barry, and Joint Nature Conservation Committee (Great Britain), eds. Palaeozoic palaeobotany of Great Britain. Chapman & Hall, 1995.

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E, Gordon J., Crofts Roger, and Scottish Natural Heritage (Agency : Great Britain), eds. Land of mountain and flood: The geology and landforms of Scotland. Birlinn, 2007.

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Cox, F. C. Geology of the country around Norwich: Memoir for 1:50 000 geologicalsheet 161 (England and Wales). H.M.S.O., 1989.

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Johnstone, G. S. The Northern Highlands of Scotland. 4th ed. H.M.S.O, 1989.

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Cox, F. C. Geologyof the country around Norwich: Memoir for 1:50 000 geologicl sheet 161 (England and Wales). H.M.S.O., 1989.

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J, Williams B., Cornwell J. D, and British Geological Survey, eds. Geology of the country around Taunton and the Quantock Hills. Natural Environment Research Council, 1985.

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McAdam, A. D. Geology of the Haddington district: Memoir for 1,50000 sheet 33W and part of sheet 41. H.M.S.O., 1985.

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Book chapters on the topic "Geology - Great Britain - Worksop"

1

Blake, Ronald N. E. "Geoenvironmental factors in the regeneration of military airfields in Great Britain." In Reviews in Engineering Geology. Geological Society of America, 2001. http://dx.doi.org/10.1130/reg14-p203.

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Zalasiewicz, Jan. "6. Geological fieldwork." In Geology: A Very Short Introduction. Oxford University Press, 2018. http://dx.doi.org/10.1093/actrade/9780198804451.003.0006.

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The rare, exotic, and wonderful has been one of the great attractions of geology, often being the ‘hook’ that initially attracted the attention of many a geological enthusiast. Dating back to at least Greek and Roman times, explorers went in search of mammoth and dinosaur bones, and prospectors targeted precious gems and metal ores. ‘Geological fieldwork’ explains, though, that systematically working out the total geology of a landscape requires a very different approach. It outlines the work of William Smith, who from the late 18th century produced the first geological maps of Great Britain, and describes some of the new technology used in modern geological fieldwork.
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Hingley, Richard. "‘The Roman occupation of Britain and our own occupation of India’." In The Recovery of Roman Britain 1586-1906. Oxford University Press, 2008. http://dx.doi.org/10.1093/oso/9780199237029.003.0009.

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The late eighteenth and early nineteenth centuries were a time of significant social change, with the industrialization of society and a massive increase in population, but there was no sudden transformation of ideas about Roman Britain. During this period, significant new archaeological finds came to light as a result of development associated with the industrialization of society, including the excavation of quarries, the construction of sewers, canals, and railways, while deep ploughing located further buried remains in the countryside. Writing in 1849, Charles Tucker suggested that the scale of development since the mid 1820s had contributed ‘so extensively to more certain knowledge of the habits and manners of the early occupants’ of Britain. Improvements in public transport resulted in a wider popular interest in the past, with the creation of national and regional archaeological societies, including the British Archaeological Association, which held its first meeting in 1844. These new organizations held meetings at which antiquaries could discuss archaeological discoveries, while the published proceedings disseminated knowledge. The realization of the antiquity of the human race brought about a serious and sustained challenge to the biblical story of creation during the middle of the nineteenth century. Gradually, with the developing knowledge of geology, ‘prehistory’ was seen to represent a great depth of time and this made it possible to conceive of a chronologically based understanding of the ‘primeval’ past. Understandings of Roman Britain, however, were slower to change, since they were based on more firmly established roots derived from centuries of study of classical texts, artefacts, and sites. Nevertheless, important discoveries helped to formulate new ideas. The period from the 1780s to 1820 was highly significant with the impressive architectural remains discovered at Bath and at a number of Roman villa sites, demonstrating the wealth of some elements of society in Roman southern Britain. The context for reflection upon these archaeological remains was transformed through the actions of British collectors in the Eastern Mediterranean who, from the 1840s, brought home classical monuments and artefacts for display in the British Museum. A renewed focus of interest in ‘the Roman Wall’ developed in the mid nineteenth century, while significant new work was undertaken on the buried Roman remains at London, Cirencester, Silchester, and Verulamium.
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Beerling, David. "Global warming ushers in the dinosaur era." In The Emerald Planet. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780192806024.003.0012.

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Reverend William Buckland (1784–1856), a British vicar and palaeontologist, was the first Professor of Geology at the University of Oxford (1813) (see Plate 8). Charming and eloquent, Buckland was also an accomplished lecturer. His biographer summed him up rather well, remarking in 1894 ‘it is impossible to convey to the mind of any one who had never heard Dr. Buckland speak, the inimitable effect of that union of the most playful fancy with the most profound reflections which so eminently characterized his scientific oratory’. Brilliant and famously eccentric, he once offended stuffier colleagues at a British Association meeting in Bristol by strutting around the lecture theatre imitating chickens to demonstrate how prehistoric birds could have left footprints in the mud. On another occasion he: . . . attracted an audience totalling several thousand for a lecture in the famous Dudley Caverns, specially illuminated for the purpose. Carried away by the general magnificence, he was tempted into rounding off with a shameless appeal to the audience’s patriotism. The great mineral wealth lying around on every hand, he proclaimed, was no mere accident of nature; it showed rather, the express intention of Providence that the inhabitants of Britain should become, by this gift, the richest and most powerful nation on Earth. And with these words, the great crowd, with Buckland at its head, returned towards the light of day thundering out, with one accord, ‘God save the Queen!’. . . Buckland also claimed to have eaten his way straight through the animal kingdom as he studied it and, allegedly, part of Louis XIV’s embalmed heart, pinched from the snuffbox of his friend the Archbishop of Canterbury. He was aided in the eccentric culinary consumption of animals by his son Francis Buckland (1826–80), the celebrated Victorian naturalist and one-time Inspector of Her Majesty’s Salmon Fisheries, who evidently inherited his father’s eccentricity. Francis Buckland lived amongst beer-swilling monkeys, rats, and hares and regarded firing benzene at cockroaches through syringes as a fine sport. Francis arranged with London Zoo to receive off-cuts from the carcasses of unfortunate animals.
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