Feldspars and Their Reactions 1994
DOI: 10.1007/978-94-011-1106-5_8
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Recent Work on Oscillatory Zoning in Plagioclase

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Cited by 42 publications
(38 citation statements)
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“…It is characterized [63,64] by variations in the anorthite content of typically 5-15% over a scale of tens to hundreds of micrometres. By plotting the thickness of one zone as a function of the previous one (first-return map), Higman & Pearce [64] suggested that an intrinsic dynamics is at least partly responsible for the formation of OZ, without precluding the influence of systematic or random changes in the external growth conditions.…”
Section: Oscillatory Zoning Patternsmentioning
confidence: 99%
See 1 more Smart Citation
“…It is characterized [63,64] by variations in the anorthite content of typically 5-15% over a scale of tens to hundreds of micrometres. By plotting the thickness of one zone as a function of the previous one (first-return map), Higman & Pearce [64] suggested that an intrinsic dynamics is at least partly responsible for the formation of OZ, without precluding the influence of systematic or random changes in the external growth conditions.…”
Section: Oscillatory Zoning Patternsmentioning
confidence: 99%
“…OZ in plagioclase occurs often in far-from-equilibrium conditions (large undercooling) [63]. L'Heureux and co-workers [71][72][73] have proposed an isothermal nonlinear model of OZ in plagioclase for such a situation.…”
Section: Oscillatory Zoning Patternsmentioning
confidence: 99%
“…There is a large literature on oscillatory zoning and its origin in igneous minerals, especially plagioclase (see reviews by Pearce 1994;Shore and Fowler 1996). Although often attributed to external factors such as variations in temperature or pressure, magma composition, P H 2 O ; etc.…”
Section: P Contents Of Igneous Olivines: Comparison To the Literaturementioning
confidence: 99%
“…Although this would result in a zone of high-P olivine overgrown by low-P olivine, something else must occur to stimulate another phase of rapid olivine growth so as to produce oscillatory zoning. Examples of how non-linearities resulting in oscillatory behavior might be introduced into the system include dependence of growth rate on the composition of the crystalline phase or on the structure of the interface and its temporal evolution, variations in the diffusivities of cations in the melt as a function of liquid composition, time dependence of the degree of constitutional supercooling of the liquid at the crystal interface, and convective instability of the liquid boundary layer (see reviews by Pearce 1994;Shore and Fowler 1996).…”
Section: P Contents Of Igneous Olivines: Comparison To the Literaturementioning
confidence: 99%
“…Of special interest in magmatic systems is compositional zoning in plagioclase which has two characteristic scales [28]. Type I zoning is smallscale, generally in the range 1^10 Wm, and has been shown to be the result of a deterministic process [26].…”
Section: Crystal Zoningmentioning
confidence: 99%