Mineralogy, Geochemistry and Tectonic Setting of the Raobazhai Ultramafic Complex, North Dabie
نویسندگان
چکیده
The Raobazhai ultramafic complex is located in the north of Dabie Mountains and composed spinel peridotites accompanied by a few lenticular mafic metamorphic rocks. are mostly harzburgite, along with minor dunite lherzolite. This study reports petrological, geochemical, Re-Os isotopic data chromite harzburgites from Raobazhai. major trace whole-rock geochemistry characteristics indicate that rocks remnants partial melting to different degrees (6–17%). Both mineral showed typical abyssal peridotite affinity. Due presence water-bearing minerals, Sr, Ba, U were enriched, Nb, Zr, Hf depleted, which can be attributed strong metasomatism boninitic melting/fluid fore-arc domain. flat distribution platinum group elements (PGE) decoupling Pt-Pd also result interaction. 187Os/188Os ratios (0.1149–0.1266) generally lower than recommended value primitive mantle fell within isotope range. indicated likely oceanic underwent transformation event.
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ژورنال
عنوان ژورنال: Minerals
سال: 2022
ISSN: ['2075-163X']
DOI: https://doi.org/10.3390/min12030286