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Journal articles on the topic 'Weald'

Author: Grafiati
Published: 4 June 2021
Last updated: 25 January 2023

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1

Jarzembowski, E. A. "New insects from the Weald Clay of the Weald." Proceedings of the Geologists' Association 102, no. 2 (January 1991): 93–108. http://dx.doi.org/10.1016/s0016-7878(08)80069-7.

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2

Jarzembowski, E. A. "The Weald Clay of the Weald: report of 1988/89 field meetings." Proceedings of the Geologists' Association 102, no. 2 (January 1991): 83–92. http://dx.doi.org/10.1016/s0016-7878(08)80068-5.

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3

Hansen, David Lundbek, Søren Bom Nielsen, and Derek J. Blundell. "A Model for the evolution of the Weald." Bulletin of the Geological Society of Denmark 49 (December 2, 2002): 109–18. http://dx.doi.org/10.37570/bgsd-2003-49-09.

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The Weald Basin developed through the Jurassic–Lower Cretaceous as an extensional basin founded upon E–W trending low-angle faults that were probably Variscan thrusts, subsequently reactivated as normal faults. Later, the basin was inverted and uplifted into a broad dome, whilst the London Basin to the north, and the Hampshire–Dieppe Basin to the south, subsided as flanking basins during the late Palaeocene–Eocene. Seismic sections across the Weald indicate that inversion resulted from north-directed stress. A stratigraphic reconstruction based on a N–S profile across the Weald and flanking basins serves as a template for a forward, 2D thermo-mechanical model that simulates the evolution of the Weald Basin through crustal extension and its inversion, and subsidence of the flanking basins, through compression. The model provides a physical explanation for this sequence of events, requiring a region of crust of reduced strength relative to its flanks. This weak region is the location of crustal-scale Variscan thrusts that have been reactivated subsequently. The strong crust on the flanks is essential for the development of flanking basins during inversion and uplift of the Weald.
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4

Hammersley, G., Henry Cleere, and David Crossley. "The Iron Industry of the Weald." Economic History Review 39, no. 2 (May 1986): 295. http://dx.doi.org/10.2307/2596154.

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5

Cleland, J. H., H. Cleere, and D. Crossley. "The Iron Industry of the Weald." Britannia 18 (1987): 385. http://dx.doi.org/10.2307/526467.

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6

Allen, J. R. L. "A Whetstone of Wealden Sandstone from the Roman Villa at Great Holts Farm, Boreham, Essex." Britannia 46 (July 14, 2015): 247–51. http://dx.doi.org/10.1017/s0068113x15000318.

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AbstractExcavated in 1992–4, the villa yielded a portion of a whetstone which, on the basis of general shape, the presence of rebated long edges and microscopic petrography in thin-section, was with little doubt made from a sandstone in the Weald Clay Formation (Lower Cretaceous) of the north-west Weald. It is representative of a widely recorded, major stone-based industry in Roman Britain, with finds known to range from the Channel coast to the northern frontier zone.
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7

Tsang, Kin Shun, John H. L. Pang, and Hsin Jen Hoh. "Influence of Weld Toe Radii on Fatigue Life Prediction." MATEC Web of Conferences 165 (2018): 22025. http://dx.doi.org/10.1051/matecconf/201816522025.

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A study was carried out to investigate the influence of the weld toe radii on the fatigue strength of butt welded joints loaded in bending and tension. Fatigue analysis starting from weld toe cracks in marine and offshore welded pipe specimens were conducted using cut-out four-point bend fatigue test specimens. Fatigue life can be enhanced by reducing the local stress concentration generated by weld toe radius effects. This study investigated the effect of different weld toe radii on the stress intensity factor at the region of the weld toe through Finite Element Analysis (FEA). FEA was used to model a butt welded steel plate extracted from a pipe subject to tension and four-point bend loading. Semi-elliptical surface (SESC) cracks were modeled at the weld toe region with different SESC crack depth and surface crack length. Four weld toe radii and two modes of loading were investigated. The stress intensity factors, weald toe magnification factors, or Mkc and Mka are reported and used for fatigue life prediction.
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8

Radley, Jonathan D. "A Wealden guide I: the Weald Sub-basin." Geology Today 22, no. 3 (May 2006): 109–18. http://dx.doi.org/10.1111/j.1365-2451.2006.00563.x.

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9

Jones, David K. C. "On the uplift and denudation of the Weald." Geological Society, London, Special Publications 162, no. 1 (1999): 25–43. http://dx.doi.org/10.1144/gsl.sp.1999.162.01.03.

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10

Benton, Ted. "Nature and People in the Weald of England." Capitalism Nature Socialism 31, no. 3 (June 29, 2020): 141–43. http://dx.doi.org/10.1080/10455752.2020.1778243.

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11

Burnside, Niall G., Dan J. Metcalfe, Roger F. Smith, and Steve Waite. "Ghyll Woodlands of the Weald: Characterisation and Conservation." Biodiversity and Conservation 15, no. 4 (April 2006): 1319–38. http://dx.doi.org/10.1007/s10531-005-3875-5.

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12

Allen, J. R. L. "The Whetstones from Roman Silchester at Reading Museum: The Victorian-Edwardian Excavations." Hampshire Studies 73, no. 1 (November 1, 2018): 156–68. http://dx.doi.org/10.24202/hs2018007.

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A hitherto undescribed assemblage of 51 whetstones recovered by Victorian-Edwardian excavators is reported below and assigned to geological sources. Unused/discarded roof tiles of Brownstones (Devonian, Lower Old Red Sandstone) and Pennant sandstone (high Upper Carboniferous) from the West Country were exploited for the majority of the whetstones. Some use was also made of roof tiles of Stonesfield Slate (Jurassic) from southern Oxfordshire. The only deliberately manufactured whetstones came from the Weald Clay Formation (Lower Cretaceous) of the northwest Weald, and from another Jurassic source in the west/south Midlands. A few whetstones, of sarsen and Bunter Pebble Beds quartzite, appear to have been 'found' objects. The Museum group is similar to the multi-period assemblage from Insula IX at Silchester, but is likely to emphasize circumstances in the town (especially the forum-basilica) during the later Roman period. A Catalogue of the whetstones is presented.
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13

Barshep, Dinfa Vincent, and Richard Henry Worden. "Reservoir Quality of Upper Jurassic Corallian Sandstones, Weald Basin, UK." Geosciences 11, no. 11 (October 29, 2021): 446. http://dx.doi.org/10.3390/geosciences11110446.

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The Upper Jurassic, shallow marine Corallian sandstones of the Weald Basin, UK, are significant onshore reservoirs due to their future potential for carbon capture and storage (CCS) and hydrogen storage. These reservoir rocks, buried to no deeper than 1700 m before uplift to 850 to 900 m at the present time, also provide an opportunity to study the pivotal role of shallow marine sandstone eodiagenesis. With little evidence of compaction, these rocks show low to moderate porosity for their relatively shallow burial depths. Their porosity ranges from 0.8 to 30% with an average of 12.6% and permeability range from 0.01 to 887 mD with an average of 31 mD. The Corallian sandstones of the Weald Basin are relatively poorly studied; consequently, there is a paucity of data on their reservoir quality which limits any ability to predict porosity and permeability away from wells. This study presents a potential first in the examination of diagenetic controls of reservoir quality of the Corallian sandstones, of the Weald Basin’s Palmers Wood and Bletchingley oil fields, using a combination of core analysis, sedimentary core logs, petrography, wireline analysis, SEM-EDS analysis and geochemical analysis to understand the extent of diagenetic evolution of the sandstones and its effects on reservoir quality. The analyses show a dominant quartz arenite lithology with minor feldspars, bioclasts, Fe-ooids and extra-basinal lithic grains. We conclude that little compactional porosity-loss occurred with cementation being the main process that caused porosity-loss. Early calcite cement, from neomorphism of contemporaneously deposited bioclasts, represents the majority of the early cement, which subsequently prevented mechanical compaction. Calcite cement is also interpreted to have formed during burial from decarboxylation-derived CO2 during source rock maturation. Other cements include the Fe-clay berthierine, apatite, pyrite, dolomite, siderite, quartz, illite and kaolinite. Reservoir quality in the Corallian sandstones show no significant depositional textural controls; it was reduced by dominant calcite cementation, locally preserved by berthierine grain coats that inhibited quartz cement and enhanced by detrital grain dissolution as well as cement dissolution. Reservoir quality in the Corallian sandstones can therefore be predicted by considering abundance of calcite cement from bioclasts, organically derived CO2 and Fe-clay coats.
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14

Ogura, M. "The Grammaticalization of the Old English Imperatives weald and loca." Notes and Queries 58, no. 1 (January 12, 2011): 10–14. http://dx.doi.org/10.1093/notesj/gjq246.

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15

Pullan, Christopher P., and Malcolm Butler. "Paleozoic gas potential in the Weald Basin of southern England." Geological Society, London, Special Publications 471, no. 1 (March 22, 2018): 333–63. http://dx.doi.org/10.1144/sp471.1.

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16

WAKO, Tatsuo. "The Natural History of Oak in Low Weald, Southeast England." Kikan Chirigaku 59, no. 4 (2007): 219–22. http://dx.doi.org/10.5190/tga.59.219.

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17

Akinlotan, Oladapo. "Mineralogy and palaeoenvironments: the Weald Basin (Early Cretaceous), Southeast England." Depositional Record 3, no. 2 (August 20, 2017): 187–200. http://dx.doi.org/10.1002/dep2.32.

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18

Pentecost, Allan. "The weathering rates of some sandstone cliffs central Weald, England." Earth Surface Processes and Landforms 16, no. 1 (February 1991): 83–91. http://dx.doi.org/10.1002/esp.3290160109.

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19

Meek, Andrew, Julian Henderson, and Jane Evans. "Isotope analysis of English forest glass from the Weald and Staffordshire." Journal of Analytical Atomic Spectrometry 27, no. 5 (2012): 786. http://dx.doi.org/10.1039/c2ja10364h.

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20

Ruffell, A. H. "A note on the Weald–Atherfield Clay junction at Brook, Surrey." Proceedings of the Geologists' Association 100, no. 3 (January 1989): 409–11. http://dx.doi.org/10.1016/s0016-7878(89)80058-6.

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21

Jarzembowski, Ed A., and Jonathan D. Radley. "The Wealden of the Weald: short report of 1998 Field Meeting." Proceedings of the Geologists' Association 112, no. 1 (January 2001): 87–90. http://dx.doi.org/10.1016/s0016-7878(01)80053-5.

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22

Radley, Jonathan D. "Weald Clay (Lower Cretaceous) palaeoenvironments in south-east England: molluscan evidence." Cretaceous Research 20, no. 3 (June 1999): 365–68. http://dx.doi.org/10.1006/cres.1999.0156.

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23

Sun, S. Q., and V. P. Wright. "Peloidal fabrics in Upper Jurassic reefal limestones, Weald Basin, southern England." Sedimentary Geology 65, no. 1-2 (November 1989): 165–81. http://dx.doi.org/10.1016/0037-0738(89)90013-4.

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24

I. Iliadi, Alexander, and Anastasiia A. Fedorova. "LEXICAL EXPLICATION OF THE CONCEPT «POWER» IN OLD ENGLISH (LEXICAL AND-SEMANTIC STUDIES)." Naukovy Visnyk of South Ukrainian National Pedagogical University named after K. D. Ushynsky: Linguistic Sciences 2022, no. 34 (July 2022): 38–47. http://dx.doi.org/10.24195/2616-5317-2022-34-4.

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The paper deals with a group of Old English lexemes with the meaning ʻpowerʼ, namely: wald/weald, mund, rīki/rīce, dōm. The use of wald/weald, mund, rīki/rīce, dōm in genre-variegated original texts gives grounds for referring them to the semantic field «Law», i.e., to a very important cluster of the vocabulary of the ancient Angles and Saxons. Working with words expressing the concept of «power», the authors set the goal of analyzing the semantic nuances that differentiate the use of OE wald, mund, etc., for which they solve several research tasks: 1) find out the sources of the semantics of ʻpowerʼ; 2) determine the conditions in which the sememe ʻpowerʼ developed on the basis of other meanings (contexts and, in one case, possibly the result of the influence of Latin as the language of law). The analysis of the material gives reason to assume that the Old English contexts, where actual connections of the meanings of a single word are traced, do not always prove the fact that the sememe ʻpowerʼ appeared precisely in the Old English period, because in other ancient Germanic languages etymological analogues with a close semantic relationship are known. This fact indicates the probability of the Proto-Germanic age of the semantic shift.
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25

AKINLOTAN, OLADAPO. "Sideritic ironstones as indicators of depositional environments in the Weald Basin (Early Cretaceous) SE England." Geological Magazine 156, no. 3 (December 7, 2017): 533–46. http://dx.doi.org/10.1017/s0016756817001017.

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AbstractThe Lower Cretaceous Wealden sideritic ironstones have a wide occurrence and great potential to aid the reconstruction of the depositional environments of the Weald Basin in SE England. However, mineralogical and geochemical datasets on the ironstones are scarce in the literature. Geochemical and mineralogical data on the sideritic ironstones are presented from the Wadhurst Clay Formation within the Weald Basin. The mineralogy of the ironstones was examined using a PANalytical X'Pert Pro X-ray diffractometer and PANalytical's HighScore Plus software. Elemental composition of the ironstones was measured using a PANalytical MiniPal2 ED-XRF (benchtop X-ray spectrometer). The examination of the mineralogy of the Wealden ironstones confirms the presence of early diagenetic siderites. The trace-element assemblage shows that the sideritic ironstones are chemically pure pointing to a freshwater origin. The sideritic ironstones reveal anoxic conditions and palaeo-salinity in the basin. More generally, it is suggested that the composition of the host rocks has significant controls on the composition of sideritic ironstones in sedimentary basins. This work reinforces the importance of the composition of sideritic ironstones as useful non-traditional data for understanding the depositional settings of sedimentary basins, especially when traditional datasets are not readily available or insufficient.
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26

CLEEVELY, R. J., and S. D. CHAPMAN. "The accumulation and disposal of Gideon Mantell's fossil collections and their role in the history of British palaeontology." Archives of Natural History 19, no. 3 (October 1992): 307–64. http://dx.doi.org/10.3366/anh.1992.19.3.307.

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Through his early interest in fossils, Mantell participated in the geological exploration of the Weald and the Chalk Downs around Lewes. The material he accumulated contributed to the descriptive phase of British palaeontology and formed his notable museums at Lewes and Brighton, before its eventual acquisition by the British Museum. The nature of his collections, their significance and use in the interpretation of both vertebrate and invertebrate fossils and our knowledge of Cretaceous faunas, are discussed.
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27

Butler, Malcolm, and Christopher P. Pullan. "Tertiary structures and hydrocarbon entrapment in the Weald Basin of southern England." Geological Society, London, Special Publications 55, no. 1 (1990): 371–91. http://dx.doi.org/10.1144/gsl.sp.1990.055.01.19.

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28

Flannery Sutherland, Joseph T., Peter A. Austen, Christopher J. Duffin, and Michael J. Benton. "Leptolepid otoliths from the Hauterivian (Lower Cretaceous) Lower Weald Clay (southern England)." Proceedings of the Geologists' Association 128, no. 4 (August 2017): 613–25. http://dx.doi.org/10.1016/j.pgeola.2017.05.001.

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29

Akinlotan, Oladapo. "Multi-proxy approach to palaeoenvironmental modelling: the English Lower Cretaceous Weald Basin." Geological Journal 53, no. 1 (February 8, 2017): 316–35. http://dx.doi.org/10.1002/gj.2893.

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30

Weiss, Kenneth M. "The weald of Kent: Darwin hesitated to Ussher in a better date." Evolutionary Anthropology: Issues, News, and Reviews 20, no. 4 (July 2011): 126–30. http://dx.doi.org/10.1002/evan.20311.

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31

Matthews, D. G. "The South East England Daffodil Show, Weald of Kent Grammar School for Girls." Circa, no. 103 (2003): 54. http://dx.doi.org/10.2307/25563916.

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32

Meeson, Bob. "Rural Medieval and Transitional Housing in the Eastern High Weald 1250–c.1570." Vernacular Architecture 51, no. 1 (January 1, 2020): 155–58. http://dx.doi.org/10.1080/03055477.2020.1818173.

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33

Radley, Jonathan D., and Percival Allen. "The Wealden (non-marine Lower Cretaceous) of the Weald Sub-basin, southern England." Proceedings of the Geologists' Association 123, no. 2 (April 2012): 245–318. http://dx.doi.org/10.1016/j.pgeola.2012.01.003.

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34

Johnson, Eric D. "Moated Sites and the Production of Authority in the Eastern Weald of England." Medieval Archaeology 59, no. 1 (January 2015): 233–54. http://dx.doi.org/10.1080/00766097.2015.1119396.

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35

Chatwin, Diana, and Mark Gardiner. "Rethinking the early medieval settlement of woodlands: evidence from the western Sussex Weald." Landscape History 27, no. 1 (January 2005): 31–49. http://dx.doi.org/10.1080/01433768.2005.10594570.

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36

Jarzembowski, E. A., E. V. Yan, B. Wang, and H. Zhang. "Ommatin beetles (Insecta: Coleoptera) from the Lower Cretaceous of northeast China and southern England." Terrestrial Arthropod Reviews 6, no. 1-2 (2013): 135–61. http://dx.doi.org/10.1163/18749836-06021062.

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Lower Cretaceous beetles belonging to the extant tribe Ommatini (Coleoptera: Cupedidae: Ommatinae) are revised and six new species proposed in the extinct Eurasian genusCionocoleus:Cionocoleus tanaesp. n.,Cionocoleus olympicussp. n. (Yixian Formation, China);Cionocoleus elizabethaesp. n.,Cionocoleus watsonisp. n.,Cionocoleus minimussp. n. (Weald Clay Group, UK); andCionocoleus jepsonisp. n. (Purbeck Limestone Group, UK). New morphological data is provided forCionocoleus magicusandCionocoleus cervicalisstat. n. of whichCionocoleus planiusculusis considered a synonym (Yixian Formation).Cionocoleus punctatuscomb. n. is considered the oldest record (Upper Jurassic; Kazakhstan) of this presumably xylophagous, warm climate genus. A simple key is provided to all known species ofCionocoleus.
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37

Kirk, J. C. "Butts Cottage, Kirdford: The Conversion of Trees to Timber in The Rural Sussex Weald." Vernacular Architecture 35, no. 1 (June 2004): 12–20. http://dx.doi.org/10.1179/vea.2004.35.1.12.

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38

Pentecost, Allan. "A note on sand ripples developing in sandstone rock seepages of the Weald, UK." Earth Surface Processes and Landforms 24, no. 13 (December 1999): 1257–59. http://dx.doi.org/10.1002/(sici)1096-9837(199912)24:13<1257::aid-esp57>3.0.co;2-f.

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39

Casanovas-Cladellas, María Lourdes, José Vicente Santafé-Llopis, and Carles Santisteban-Bové. "Dacentrurus armatus (Stegosauria, Dinosauria) del Cretácico Inferior de los Serranos (Valencia, España)." Spanish Journal of Palaeontology 10, no. 2 (August 9, 2022): 273. http://dx.doi.org/10.7203/sjp.24155.

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La localidad de "Cerrito del Olmo", situada cerca de la aldea de la Almeza (Valencia, España) ha proporcionado diversos restos de estegosaurios: vértebras cervicales, dorsales y caudales, costillas y un fragmento de isquion. Las características morfológicas de las vértebras cervicales, con las costillas cervicales fusionadas, y la morfología de la cara anterior de las vértebras dorsales, nos han permitido asignarlo a Dacentrurus armatus. Los materiales que aparecen en "Cerrito del Olmo" son un conjunto de paleocanales de areniscas intercaladas con margas grises y arcillas rojas que se incluyen en la base del tramo B de los materiales de facies Weald del, sector denominado "Cubeta de Aras de Alpuente" (Hauteriviense superior-Barremiense inferior).
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40

Pentecost, Allan. "The freshwater-algal flora of the Kent and Sussex Weald, UK: 160 years of change." Archiv für Hydrobiologie 163, no. 2 (June 1, 2005): 259–85. http://dx.doi.org/10.1127/0003-9136/2005/0163-0259.

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41

Taylor, Kevin G. G. "Pedogenic clay–mineral transformation in the Weald Basin: implications for Early Cretaceous hinterland climate reconstructions." Cretaceous Research 17, no. 1 (February 1996): 103–8. http://dx.doi.org/10.1006/cres.1996.0008.

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42

Chamberlin, Elizabeth. "Medieval Villages in the Eastern High Weald 1250–1750: The Villages Explained, part 1 and 2." Vernacular Architecture 49, no. 1 (January 2018): 158–59. http://dx.doi.org/10.1080/03055477.2018.1525892.

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43

Abbott, Sunshine S., Cédric M. John, and Alastair J. Fraser. "Detailed 3-D depositional architecture of Late Jurassic carbonate–anhydrite cycles (Brightling Mine, Weald Basin, UK)." Marine and Petroleum Geology 69 (January 2016): 74–93. http://dx.doi.org/10.1016/j.marpetgeo.2015.10.012.

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44

Qing Sun, S. "A storm-dominated offshore sandstone interval from the Corallian Group (Upper Jurassic), Weald Basin, southern England." Marine and Petroleum Geology 9, no. 3 (June 1992): 274–86. http://dx.doi.org/10.1016/0264-8172(92)90076-q.

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45

Hawkes, P. W., A. J. Fraser, and C. C. G. Einchcomb. "The tectono-stratigraphic development and exploration history of the Weald and Wessex basins, Southern England, UK." Geological Society, London, Special Publications 133, no. 1 (1998): 39–65. http://dx.doi.org/10.1144/gsl.sp.1998.133.01.03.

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46

TAYLOR, STEVE P., BRUCE W. SELLWOOD, RAMUES W. GALLOIS, and MARTIN H. CHAMBERS. "A sequence stratigraphy of the Kimmeridgian and Bolonian stages (late Jurassic): Wessex–Weald Basin, southern England." Journal of the Geological Society 158, no. 1 (January 2001): 179–92. http://dx.doi.org/10.1144/jgs.158.1.179.

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47

Widdicombe, R. C. "WOODLAND CHANGE AND THE DENDROCHRONOLOGY OF FAGUS SYLVATICA IN A PLATEAU BEECH WOOD OF THE WEALD." Arboricultural Journal 20, no. 1 (February 1996): 79–93. http://dx.doi.org/10.1080/03071375.1996.9747103.

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48

Ross, Andrew J., and Elizabeth Cook. "The stratigraphy and palaeontology of the Upper Weald Clay (Barremian) at Smokejacks Brickworks, Ockley, Surrey, England." Cretaceous Research 16, no. 6 (December 1995): 705–16. http://dx.doi.org/10.1006/cres.1995.1044.

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49

Hill, C. R. "A plant with flower-like organs from the Wealden of the Weald (Lower Cretaceous), southern England." Cretaceous Research 17, no. 1 (February 1996): 27–38. http://dx.doi.org/10.1006/cres.1996.0003.

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50

Mansy, J. L., G. M. Manby, O. Averbuch, M. Everaerts, F. Bergerat, B. Van Vliet-Lanoe, J. Lamarche, and S. Vandycke. "Dynamics and inversion of the Mesozoic Basin of the Weald–Boulonnais area: role of basement reactivation." Tectonophysics 373, no. 1-4 (September 2003): 161–79. http://dx.doi.org/10.1016/s0040-1951(03)00289-0.

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