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《Geochimica》 2003-02
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Optimized geospeedometry: Evidence for slow cooling of the Huangtuling granulite, northern Dabie Mountains

P>CHENG Hao1, CHEN Dao gong1, Weiji CHENG2, WU Yuan bao1, HUANG Sheng1<P>(1. School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China; 2. Department of Geosciences, University of Arizona, Tucson AZ 85721, USA)<P>  
Compositions of a large number of garnet crystals in the Huangtuling granulite from the northern Dabie Mountains are determined with electron microprobe, and garnet zoning is observed. Detailed and careful step scanning across a couple of selected garnet biotite is performed. With our developed diffusion model, the profile is numerically modeled. The result suggests the rocks of the Huangtuling granulite suffered a very slow cooling about 0.1 ℃ /a after the granulite phase. A cooling rate from garnet zoning in the Dabie Mountains is derived.P
【Fund】: 国家自然科学基金(40273028)
【CateGory Index】: P595
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