The use of palaeo-flow direction indicators in basaltic lavas in landscape history reconstruction: A reconnaissance study and evaluation from northern New South Wales, Australia

1993 ◽  
Vol 37 (2) ◽  
pp. 157-170
Author(s):  
Nicola Smith ◽  
Paul Bishop
Keyword(s):  
New South ◽  
Flow Direction ◽  
New South Wales ◽  
Landscape History ◽  
South Wales ◽  
Basaltic Lavas

Residual glasses from some alkali basaltic lavas from New South Wales

1966 ◽  
Vol 35 (274) ◽  
pp. 847-860 ◽  
Author(s):  
J. F. G. Wilkinson
Keyword(s):  
New South ◽  
Olivine Basalt ◽  
New South Wales ◽  
South Wales ◽  
Alkali Olivine Basalt ◽  
Host Rocks ◽  
Basaltic Lavas

SummaryThe glassy residua from an alkali olivine-basalt and a nephelinebasanite are respectively alkali trachytic and phonolitic in composition and contrast strongly with the compositions of the host rocks. The analysis of the glass from the alkali olivine-basalt reveals appreciable normative corundum, which is considered a consequence of the crystallization of excessive diopsidic clinopyroxene. This results in a deficiency in lime relative to alumina during the crystallization of much of the plagioclase. A consideration of the compositions of the glasses and the salic differentiates from alkaline basic intrusions indicates that the development of either trachyte or phonolite depends on differing degrees of undersaturation of the parental basic magmas.

Sign in / Sign up

Export Citation Format

Share Document