Pattern formation during crystallization and the formation of fine-scale layering.
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, Journal Article
Boudreau, AE
Published in: Origins of igneous layering
January 1, 1986
Fine-scale layering is characterized by the laminar segregation of mineral phases on a mm to cm scale. Where best developed, it is found in specific associations within the Stillwater Complex. In the Banded series, layer spacing is proportional to crystal grain size, with the best examples of fine-scale layering characterized by coarse rock textures and the development of secondary structures. Quantitative modeling can explain many of the features of fine- scale layering, and suggests that textural features of igneous layering in general can become better defined with time.-from Author
Duke Scholars
Published In
Origins of igneous layering
Publication Date
January 1, 1986
Start / End Page
453 / 471
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Boudreau, A. E. (1986). Pattern formation during crystallization and the formation of fine-scale layering. Origins of Igneous Layering, 453–471.
Boudreau, A. E. “Pattern formation during crystallization and the formation of fine-scale layering.” Origins of Igneous Layering, January 1, 1986, 453–71.
Boudreau AE. Pattern formation during crystallization and the formation of fine-scale layering. Origins of igneous layering. 1986 Jan 1;453–71.
Boudreau, A. E. “Pattern formation during crystallization and the formation of fine-scale layering.” Origins of Igneous Layering, Jan. 1986, pp. 453–71.
Boudreau AE. Pattern formation during crystallization and the formation of fine-scale layering. Origins of igneous layering. 1986 Jan 1;453–471.
Published In
Origins of igneous layering
Publication Date
January 1, 1986
Start / End Page
453 / 471