This is a preprint, the final version is subject to change, of the American Mineralogist (MSA) Cite as Authors (Year) Title. American Mineralogist, in press. (DOI will not work until issue is live.) DOI: http://dx.doi.org/10.2138/am.2013.4494 6/19 1 Revision 1 2 3 Extreme fractionation from zircon to hafnon in the Koktokay No. 4 1 granitic pegmatite, Altai, northwestern China 5 6 Rong Yin1, Ru Cheng Wang1,*, Ai-Cheng Zhang1, Huan Hu1, Jin Chu Zhu1, Can Rao2, and 7 Hui Zhang3 8 9 1State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and 10 Engineering, Nanjing University, Nanjing 210093, China; 11 2Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China; 12 3Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, 550002, China. 13 14 *E-mail:
[email protected] 15 Always consult and cite the final, published document. See http://www.minsocam.org or GeoscienceWorld This is a preprint, the final version is subject to change, of the American Mineralogist (MSA) Cite as Authors (Year) Title. American Mineralogist, in press. (DOI will not work until issue is live.) DOI: http://dx.doi.org/10.2138/am.2013.4494 6/19 16 ABSTRACT 17 The Koktokay No. 1 pegmatite is a Li–Cs–Ta-rich granitic pegmatite located in Altai, 18 northwestern China. Zircon is present in most textural zones of this pegmatite and in its 19 contact zone with surrounding metagabbro. Here we describe the detailed associations of 20 zircon with other minerals, and the internal textures and chemistry of the zircons.