Title: Alteration of magmatic monazite in granitoids from the Ryoke belt (SW Japan): processes and consequences Manuscript Number: 7025R - CORRECTION Authors: Etienne Skrzypek, University of Graz Shuhei Sakata, Gakushuin University Dominik Sorger, University of Graz 1 Alteration of magmatic monazite in granitoids from the Ryoke belt (SW Japan): 2 processes and consequences 3 4 REVISION 1 st 5 Corrected October 31 2019 6 1,2* 3 2 7 ETIENNE SKRZYPEK , SHUHEI SAKATA AND DOMINIK SORGER 8 1Department of Geology and Mineralogy, Graduate School of Science, Kyoto University, 9 Kitashirakawa-Oiwakecho, Sakyo-ku, Kyoto 606-8502, Japan 10 2Department of Petrology and Geochemistry, NAWI Graz Geocenter, University of Graz, 11 Universitätsplatz 2, 8010 Graz, Austria 12 3Department of Chemistry, Faculty of Science, Gakushuin University, 1-5-1 Mejiro, Toshima- 13 ku, Tokyo 171-8588, Japan 14 * E-mail:
[email protected] 15 16 Running title: Alteration of magmatic monazite 17 18 With 7 figures and 2 tables 19 1 1 20 ABSTRACT 21 The alteration of magmatic monazite and its consequences for monazite geochronology are 22 explored in granitoids from the western part of the Ryoke belt (Iwakuni-Yanai area, SW 23 Japan). Biotite-granite samples were collected in two plutons emplaced slightly before the 24 main tectono-metamorphic event: one, a massive granite (Shimokuhara) adjoins schistose 25 rocks affected by greenschist facies metamorphism; and the second, a gneissose granite 26 (Namera) adjoins migmatitic gneiss that experienced upper-amphibolite facies conditions. 27 Despite contrasting textures, the granite samples have similar mineral modes and 28 compositions. Monazite in the massive granite is dominated by primary domains with limited 29 secondary recrystallization along cracks and veinlets.