Abstract

An investigation has been made of the chemical and mineralogical transformations which have accompanied the weathering of six basic volcanic rocks from eastern New South Wales. Montmorillonite is initially formed from the destruction of the olivine, pyroxene, and plagioclase in the parent rock, but, in the near-surface horizons, this mineral is unstable and may form kaolinite, halloysite, or a poorly crystalline montmorillonite. The alumina content shows a steady increase up the profiles, whereas the alkalis, alkaline earths, and some of the silica have been lost in the ground-waters during the mineral transformations. Marked concentrations of iron and titanium occur at specific levels in some of the weathering profiles and explanations of these phenomena are given.

Keywords

WeatheringHalloysiteKaolinitePlagioclaseGeologyMontmorilloniteGeochemistryMineralClay mineralsOlivineVolcanoMineralogyParent rockChemistryMetallurgyQuartzMaterials science

Related Publications

Publication Info

Year
1964
Type
article
Volume
2
Issue
2
Pages
218-234
Citations
100
Access
Closed

External Links

Social Impact

Social media, news, blog, policy document mentions

Citation Metrics

100
OpenAlex

Cite This

D.C. Craig, F. C. Loughnan (1964). Chemical and mineralogical transformations accompanying the weathering of basic volcanic rocks from New South Wales. Australian Journal of Soil Research , 2 (2) , 218-234. https://doi.org/10.1071/sr9640218

Identifiers

DOI
10.1071/sr9640218