Magnesioferrite-rich spinels were found in the Cretaceous Jianguo trachyandesite in northeastern China. The trachyandesite is comprised of augite, plagioclase, K-feldspar, spinel, phlogopite, apatite, zircon, and pseudo- morphed phenocrysts, which are interpreted as former olivine and/or orthopyroxene crystals and now consist of a mixture of chrysotile, antigorite and chlorite. Texturally, four stages of spinel growth are observed: magnesioferrite- rich spinel-I occurs within the pseudomorphs and magne- sioferrite-rich spinel-II occurs in the matrix of the trachyandesite. Magnetite-rich spinel-III occurs either as rim around spinel-II or as distinct magnetite grains, whereas worm—like magnetite—rich spinel-IV occurs within the pseudomorphs. Chemically, spinel-I contains 51 to 82 mol.% magnesioferrite component, spinel-II contains a magnesio- ferrite component ranging from 60 to 79 mol% and spinel-III contains less than 15 mol.% magnesioferrite component. In contrast to spinel II, spinel-I is poor in TiO2 but rich in Cr2O3, MnO and NiO. Two-feldspar thermometry yields temperatures of 880-1000°C for the formation of the trachyandesite matrix assemblage. In the absence of olivine and/or orthopyroxene, Schreinemakers analysis of T-fO2 model phase relations indicate that magnesioferrite-rich spinels-I, and II are stable at high T and high fO2. Magnetite-rich spinel-III formed under more reducing conditions, while spinel-IV most likely formed during subsolidus late-stage alteration of olivine and/or magnesio- ferrite phenocrysts. Semi quantitative fO2 calculations using the oxygen barometer of Ballhaus et al. (1991) yielded fO2 >7 log units above QFM, which excludes a mantle origin of these magnesioferrites. Thus oxidation of these trachyandesites most likely occurred at some stage during melt ascent, or in a differentiating magma chamber or even after emplacement of these still hot magmas at near surface conditions.
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