Fluid-induced alteration of monazite, magnetite, and sulphides during the albitization of a Palaeoproterozoic granite from the Jiao-Liao-Ji orogenic belt, North China Craton

Hellandite-(Y)–hingganite-(Y)–fluorapatite retrograde coronae: a novel type of fluid-induced dissolution–reprecipitation breakdown of xenotime-(Y) in the metagranites of Fabova Hoľa, Western Carpathians, Slovakia

“…For example, the commonly observed breakdown of monazite-(Ce) includes a subsolidus retrograde corona around its partly dissolved core with distinctive concentric mineral zones of apatite ± Th-silicate/oxide, and allanite-(Ce) to REE-rich epidote or clinozoisite (e.g. Broska and Siman, 1998; Finger et al , 1998, 2016; Budzyń et al , 2010; Ondrejka et al , 2012, 2016; Upadhyay and Pruseth, 2012; Lo Pò et al , 2016; Ji et al , 2021). This micro-texture is documented mostly in low- to medium-temperature metagranitoids with primary magmatic monazite-(Ce).…”