The term ‘locked sand’ has been introduced by Dusseault & Morgenstern to distinguish the characteristics of certain, geologically old, natural sands from recently deposited and compacted sands. They examined three North American Sands in detail and described their main characteristics. The work described here is a similar investigation of two English Tertiary Sands to discover whether or not they have similar characteristics. It is shown that the Bagshot and Barton Sands correspond in respect of lack of a cement, an in situ relative density greater than 100% and the ability to be sampled as intact, undisturbed blocks. They are, however, slightly less dense and notably less strong than the North American Sands described by Dusseault &...
Sands of the Mallee Dunefield, south-eastern Australia, are divided into two groups on the basis of ...
Findings of a fundamental study of the mechanical consequences of internal erosion are reported from...
The Upper Greensand of south-west England can be divided on bulk lithology into two roughly equal pa...
The Folkestone Beds formation is a marine shallow-water deposit of Cretaceous age. It consists mostl...
This is an Engineering Geological study of the arenaceous members of the Lower Greensand (Lower Cret...
Values of relative density (Dr) have been measured on 20 samples of uncemented, virtually matrix-fre...
Quantifying the fabric of intact soil is of great importance in both geomechanics and geology. A uni...
Studies of the extent of diagenetic change in matrix-free, uncemented, quartzose sands ranging in ag...
Abstract — The geotechnical properties of the Barton Clay from the Hampshire Basin in England are pr...
After a long period of neglect there has been increasing interest in the sand/sandstone borderline m...
Sands and sandstones from Leg 66 of the Deep Sea Drilling Project can be grouped into three general ...
International audienceA comparison of the behavior of uncemented and grouted sands is presented. Fou...
Direct shear tests up to 10 MPa normal stress have been carried out on two sets of intact block samp...
Natural soil deposits are likely to have a structure resulting from particle bonding or interlocking...
Abstract: Up to the present, exploration of the UK Lower Cretaceous deep-water sand-stone play has b...
Sands of the Mallee Dunefield, south-eastern Australia, are divided into two groups on the basis of ...
Findings of a fundamental study of the mechanical consequences of internal erosion are reported from...
The Upper Greensand of south-west England can be divided on bulk lithology into two roughly equal pa...
The Folkestone Beds formation is a marine shallow-water deposit of Cretaceous age. It consists mostl...
This is an Engineering Geological study of the arenaceous members of the Lower Greensand (Lower Cret...
Values of relative density (Dr) have been measured on 20 samples of uncemented, virtually matrix-fre...
Quantifying the fabric of intact soil is of great importance in both geomechanics and geology. A uni...
Studies of the extent of diagenetic change in matrix-free, uncemented, quartzose sands ranging in ag...
Abstract — The geotechnical properties of the Barton Clay from the Hampshire Basin in England are pr...
After a long period of neglect there has been increasing interest in the sand/sandstone borderline m...
Sands and sandstones from Leg 66 of the Deep Sea Drilling Project can be grouped into three general ...
International audienceA comparison of the behavior of uncemented and grouted sands is presented. Fou...
Direct shear tests up to 10 MPa normal stress have been carried out on two sets of intact block samp...
Natural soil deposits are likely to have a structure resulting from particle bonding or interlocking...
Abstract: Up to the present, exploration of the UK Lower Cretaceous deep-water sand-stone play has b...
Sands of the Mallee Dunefield, south-eastern Australia, are divided into two groups on the basis of ...
Findings of a fundamental study of the mechanical consequences of internal erosion are reported from...
The Upper Greensand of south-west England can be divided on bulk lithology into two roughly equal pa...