Trace Element Mobility in Subducted Marble and Associated Eclogite: Constraints from UHP Rocks in the Shuanghe Area, Central-East China
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Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s12583-022-1692-3.pdf
Reference115 articles.
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2. Arculus, R. J., Lapierre, H., Jaillard, É., 1999. Geochemical Window into Subduction and Accretion Processes: Raspas Metamorphic Complex, Ecuador. Geology, 27(6): 547–550. https://doi.org/10.1130/0091-7613(1999)027>0547:GWISAA<2.3.CO;2
3. Auzanneau, E., Vielzeuf, D., Schmidt, M. W., 2006. Experimental Evidence of Decompression Melting during Exhumation of Subducted Continental Crust. Contributions to Mineralogy and Petrology, 152(2): 125–148. https://doi.org/10.1007/s00410-006-0104-5
4. Barth, M. G., Foley, S. F., Horn, I., 2002. Partial Melting in Archean Subduction Zones: Constraints from Experimentally Determined Trace Element Partition Coefficients between Eclogitic Minerals and Tonalitic Melts under Upper Mantle Conditions. Precambrian Research, 113(3/4): 323–340. https://doi.org/10.1016/S0301-9268(01)00216-9
5. Becker, H., Jochum, K. P., Carlson, R. W., 2000. Trace Element Fractionation during Dehydration of Eclogites from High-Pressure Terranes and the Implications for Element Fluxes in Subduction Zones. Chemical Geology, 163(1/2/3/4): 65–99. https://doi.org/10.1016/S0009-2541(99)00071-6
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