2002
DOI: 10.1016/s0016-7037(01)00792-x
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A model of oscillatory zoning in solid solutions grown from aqueous solutions: Applications to the (Ba,Sr)SO 4 system

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Cited by 35 publications
(28 citation statements)
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“… 9 , 30 , the solubility constants of the solid solution endmembers must differ by several orders of magnitude. In other work 31 33 , modeling of crystal growth at the mineral-fluid interface supports the hypothesis that compositional zonation is promoted by a difference in the endmember solubility constants of several orders of magnitude, combined with diffusion-limited solute transport at the mineral-fluid interface. In the example of (Ba, Sr)SO 4 , the solubility product constant (K sp ) values of endmembers BaSO 4 (pK sp = 9.98) 34 and SrSO 4 (pK sp = 6.63) 35 differ by three orders of magnitude.…”
Section: Introductionmentioning
confidence: 52%
“… 9 , 30 , the solubility constants of the solid solution endmembers must differ by several orders of magnitude. In other work 31 33 , modeling of crystal growth at the mineral-fluid interface supports the hypothesis that compositional zonation is promoted by a difference in the endmember solubility constants of several orders of magnitude, combined with diffusion-limited solute transport at the mineral-fluid interface. In the example of (Ba, Sr)SO 4 , the solubility product constant (K sp ) values of endmembers BaSO 4 (pK sp = 9.98) 34 and SrSO 4 (pK sp = 6.63) 35 differ by three orders of magnitude.…”
Section: Introductionmentioning
confidence: 52%
“…This difference effectively shuts down oscillatory growth of metamorphic garnet by this mechanism [ L'Heureux and Fowler , 1996]. A modified kinetic model has also been proposed for synthetic sulfates [ L'Heureux and Jamtveit , 2002], and whereas it cannot be excluded theoretically, it also cannot be tested because it involves nonmeasurable terms.…”
Section: Interpretation Of Oscillationsmentioning
confidence: 99%
“…It shows how porosity is modified by compaction and the reactive kinetics of the precipitation/dissolution of minerals. Equation (9) indicates that…”
Section: Mass Conservation Equationsmentioning
confidence: 99%
“…On the other hand, in a nonlinear nonequilibrium geosystem, the presence of positive feedback may result in a pattern formation that is self-organized even in an external environment that does not change (intrinsic mechanisms) [2,4]. Examples of such geochemical self-organization are found in the oscillatory zoning of solid solutions series [4,[6][7][8][9], Liesegang band formation [10][11][12][13][14][15][16][17], orbicular granites [7,18], and cyclic layering in igneous bodies [19,20].…”
Section: Introductionmentioning
confidence: 99%