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- W2074451625 abstract "The Gaijing Pb–Zn–Mo deposit and Shapinggou Mo deposit in the Yinshan region, Jinzhai, Anhui province, China, are hosted in various granitic intrusions with 40Ar/39Ar ages obtained for biotite and hornblende of 136.8 ± 1.6 Ma (medium-grained monzogranite), 130.4 ± 1.2 Ma (fine-grained granite), and 125.4 ± 1.0 Ma (fine-grained diorite). The modes of occurrence and cross-cutting relationships among the igneous intrusions indicate that alkali quartz-syenite and quartz-syenite porphyry (cryptoexplosive breccia) formed later than the calc-alkali monzogranite, granite, and diorite. Molybdenum mineralization occurs in pipe-like bodies hosted in cryptoexplosive breccia (pipe), quartz-syenite (porphyry), monzogranite, and granite, whereas Pb–Zn mineralization occurs in veins distally from the Mo mineralization. The Re–Os isotopic model ages of molybdenite from the Gaijing Pb–Zn–Mo deposit are 112.6 ± 1.3 and 113.5 ± 1.3 Ma, consistent with the ages of other molybdenum deposits throughout the East Qinling–Dabie metallogenic belt. The geological characteristics and isotopic ages of the Gaijing Pb–Zn–Mo and Shapinggou Mo deposits indicate a genetic relationship to the emplacement of the quartz-syenite (porphyry) and to shallow-seated porphyry–cryptoexplosive breccia intrusions. The present results, combined with existing data, suggest that the Pb–Zn–Mo deposits and related igneous rocks were formed in a geodynamic setting of regional lithospheric thinning, delamination, and thermal erosion in East China. The deposits are part of the East Qinling–Dabie molybdenum belt, which in turn is part of a large-scale E–W-trending metallogenic belt in East China." @default.
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- W2074451625 date "2011-12-01" @default.
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- W2074451625 title "Geochronology and tectonic setting of Pb–Zn–Mo deposits and related igneous rocks in the Yinshan region, Jinzhai, Anhui province, China" @default.
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- W2074451625 doi "https://doi.org/10.1016/j.oregeorev.2011.08.008" @default.
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