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Ostwald ripening as a possible mechanism for zircon overgrowth formation during anatexis: theoretical constraints, a numerical model, and its application to pelitic migmatites of the Tickalara Metamorphics, northwestern Australia

✍ Scribed by A.A. Nemchin; L.M. Giannini; S. Bodorkos; N.H.S. Oliver


Book ID
117116797
Publisher
Elsevier Science
Year
2001
Tongue
English
Weight
831 KB
Volume
65
Category
Article
ISSN
0016-7037

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