Ma. Woods et al., THE STRATIGRAPHY OF THE GAULT FORMATION (MIDDLE AND UPPER ALBIAN) IN THE BGS ARLESEY BOREHOLE, BEDFORDSHIRE, Proceedings of the Geologists' Association, 106, 1995, pp. 271-280
A cored borehole at Arlesey, Bedfordshire proved, in descending sequen
ce, the Lower Chalk, Cambridge Greensand, Gault, and Lower Greensand.
The macro- and microfaunas, together with lithology, are used to subdi
vide the c. 57 m thick Gault succession. Comparison with the Upper Gau
lt of the Duxford and Little Chishill boreholes indicates a possible t
ectonic influence on sediment accumulation in the Arlesey area.