A platform for research: civil engineering, architecture and urbanism
A platform for research: civil engineering, architecture and urbanism
Mineralogy of commercial dyke clays in Sydney district, N.S.W.
Residual clays formed by extensive leaching of Tertiary dikes in Sydney district are predominantly kaolinitic, though illite is present to extent of 30%; clays contain relatively high percentage of titania, much of which occurs as distinctive leucoxene octahedra, believed to be pseudo-morphous after "titaniferous magnetite"; there is association of illite with these octahedral forms of leucoxene.
Mineralogy of commercial dyke clays in Sydney district, N.S.W.
Residual clays formed by extensive leaching of Tertiary dikes in Sydney district are predominantly kaolinitic, though illite is present to extent of 30%; clays contain relatively high percentage of titania, much of which occurs as distinctive leucoxene octahedra, believed to be pseudo-morphous after "titaniferous magnetite"; there is association of illite with these octahedral forms of leucoxene.
Mineralogy of commercial dyke clays in Sydney district, N.S.W.
Roy Soc New South Wales -- J Proc
Loughnan, F.C. (author) / Golding, H.G. (author)
1957
7 pages
Plate
Article (Journal)
English
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