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Lambeth Group
Rates of oxygen-depletion in granular Lambeth Group strata and evidence for barometric pumping
Deoxygenated gas occurrences in the Lambeth Group of central London, UK
( a ) The Mid-Lambeth Group Hiatus (MLGH) exposed in the main tunnel face a...
Lambeth Group material identified within a borehole from central London; wi...
Simplified stratigraphy for the Thanet Sand Formation and Lambeth Group. Th...
Magnetostratigraphy of Upper Paleocene Through Lower Middle Eocene Strata of Northwest Europe
Abstract Ormesby Clay Formation mudstones in eastern Norfolk are the oldest upper Paleocene deposits (Chron C26r) of southern England. The base of the type Thanet Sand Formation (= start of the Thanetian Stage) is approximately 0.65 my younger (C26n). C25n is missing from the stratigraphic record across much of southern England indicating an hiatus >0.5 my between the Ormesby Clay-Thanet Sand Formations and the Lambeth Group. However, in Central London the basal unit of the Lambeth Group, the Upnor Formation, contains a record of C25n. The bulk of the Lambeth Group, the Harwich Formation and lower London Clay Formation, were all deposited during Chron C24r. The NP9/10 boundary, a commonly used Paleocene/Eocene boundary marker, is correlated with the unconformity (approximately 0.4 my) that separates the Lambeth Group from the Harwich Formation. The start of C24n.3n is positioned at the base of Division B of the London Clay and leper Clay Formations. In the Hampshire Basin, an unconformity of at least 0.66 my is marked by the absence of a record of Chron C22n.