scholarly journals Compositional Convection Trumps Silicate Liquid Immisciblity in Layered Intrusions: a Discussion of 'Liquid immiscibility and the evolution of basaltic magma' by Veksler et al., Journal of Petrology 48, 2187-2210

2008 ◽  
Vol 49 (12) ◽  
pp. 2157-2168 ◽  
Author(s):  
S. A. Morse
1983 ◽  
Vol 120 (4) ◽  
pp. 321-329 ◽  
Author(s):  
G. Lucido

Summary. Mechanisms forming silicic segregations from basaltic magmas are considered of primary importance when dealing with magmatic problems. However, the processes which give rise to silicic segregations from basaltic magmas are so far obscure. Fortunately, the discovery of spheroidal felsic masses in some basic rocks of Western Sicily throws light on this subject. To clarify the relationships between felsic and basic fractions particular attention has been paid to the interactions which occurred at their contact. Textural evidence indicates that the accretion mechanism of the Sicilian felsic segregations tends to obliterate the silicate liquid immiscibility effects and suggests that the formation of silicic segregations is a consequence of liquid unmixing phenomena.


2007 ◽  
Vol 48 (11) ◽  
pp. 2187-2210 ◽  
Author(s):  
I. V. Veksler ◽  
A. M. Dorfman ◽  
A. A. Borisov ◽  
R. Wirth ◽  
D. B. Dingwell

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