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

Details 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 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

Sep 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001gecoa..65.2771n&link_type=ejournal

Geochimica et Cosmochimica Acta, v. 65, iss. 16, p. 2771-2788.

Physics

6

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