This work presents a quantitative analysis of spatiotemporal patterns
that form during the growth of oscillatory zoned plagioclase. These pa
tterns were imaged using Nomarski interference contrast imaging of etc
hed polished surfaces. Analysis of these imaged patterns yields new in
formation and constraints on how patterns form, and consequently on ho
w oscillatory zoned crystals may develop in magmatic systems. Utilizin
g mathematical techniques recently developed for the analysis of dynam
ical systems, we show that the irregular nature of oscillatory zoning
is not compatible with random or stochastic processes. The analysis of
our observations suggests that the plagioclase-liquid system is a det
erministic nonlinear system whose attractor has a relatively low dimen
sion. Finally, comparison of our empirical results with computer model
s of other dynamical systems implies that as few as two variables may
be sufficient to describe the dynamics of the plagioclase-liquid syste
m.