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Thames River
The distributions and variations of Quaternary Thames River Terrace deposits of Greater London
Geological structures beneath the River Thames in London: findings from the Thames Tideway Tunnel investigations
Cyprideis torosa (Jones, 1850) in its type area and stratigraphical context: potential for mapping the freshwater/estuarine boundaries of the Thames–Medway river system in the MIS 9 and MIS 11 interglacials
Upper Cretaceous radiolarians reworked in the Eocene London Clay Formation, SE England
Geochemically Based Solutions for Urban Society: London, A Case Study
Groundwater reinjection and heat dissipation: lessons from the operation of a large groundwater cooling system in Central London
Controls on the basin-scale distribution of hydraulic conductivity of superficial deposits: a case study from the Thames Basin, UK
Spatial and temporal relationships between Eocene sand horizons and iron contamination in stream water in the Thames Basin west of London, UK
Sinking a jacked caisson within the London Basin geological sequence for the Thames Water Ring Main extension
An analysis of Cotswold topography: insights into the landscape response to denudational isostasy
Application of head-flow responses to groundwater floods in Chalk catchments
Assessment of standard research sand for laboratory testing
From concept towards reality: developing the attributed 3D geological model of the shallow subsurface
A framework for monitoring regional groundwater quality
Book Reviews
The history of the major rivers of southern Britain during the Tertiary
Chalk engineering geology – Channel Tunnel Rail Link and North Downs Tunnel
Estimating transmissivity from surface resistivity soundings: an example from the Thames Gravels
Abstract Realization that continental records of Quaternary rocks were more complex that hitherto believed came with the re-interpretation of oxygen isotope stratigraphy in the late 1960s and early 1970s. This necessitated a comprehensive re-evaluation that has been assisted by the emergence of new geochronological methods for terrestrial as well as land-sea correlations. The current state of such correlations is presented in this revised set of proposals for correlations in England, Ireland, Scotland and Wales, which also includes the Quaternary geology of the continental shelf. Correlation with the global standard of oxygen isotope stratigraphy enables the significance of British lithostratigraphical units to be appreciated in a wider context that includes the evolution of the climate system on the margin of the northeast Atlantic Ocean. It thus provides timely British data for the international palaeoceanographical and palaeoclimatological community and the correlations proposed are primarily on Milankovitch timescales. But their appearance coincides with the early stages of a paradigm shift to the search for both terrestrial and land-sea correlation on millennial timescales and then on centennial and decadal ones. This is the first of many similar terrestrial and land-sea correlations.