Volume 43 Issue 1
Jan.  2018
Turn off MathJax
Article Contents
Gao Yijie, Liu Jingbo, 2018. Research Advances of Melt Inclusions in High-Grade Metamorphic Rocks. Earth Science, 43(1): 236-246. doi: 10.3799/dqkx.2018.014
Citation: Gao Yijie, Liu Jingbo, 2018. Research Advances of Melt Inclusions in High-Grade Metamorphic Rocks. Earth Science, 43(1): 236-246. doi: 10.3799/dqkx.2018.014

Research Advances of Melt Inclusions in High-Grade Metamorphic Rocks

doi: 10.3799/dqkx.2018.014
  • Received Date: 2017-10-07
  • Publish Date: 2018-01-15
  • Melt inclusions in high-grade metamorphic rocks are melt drops enclosed in host minerals such as garnet and zircon, which are composed of daughter minerals, glass and other accidently trapped solid minerals. In the last decade, melt inclusions have become a new approach to the study of partial melting process in high-grade metamorphic rocks. It is generally difficult to identify and analyze melt inclusions since they are mostly less than 20 μm in diameter. This paper systematically summarizes the identification methods, microstructural features, and chemical investigation methods. The significance of melt inclusions on the identification of partial melting and constraints of the P-T condition, mechanism and fluid regime of partial melting are also discussed.

     

  • loading
  • Acosta-Vigil, A., Barich, A., Bartoli, O., et al., 2016.The Composition of Nanogranitoids in Migmatites Overlying the Ronda Peridotites (Betic Cordillera, S Spain):The Anatectic History of a Polymetamorphic Basement.Contributions to Mineralogy and Petrology, 171(3):24. https://doi.org/10.1007/s00410-016-1230-3
    Acosta-Vigil, A., Cesare, B., London, D., et al., 2007.Microstructures and Composition of Melt Inclusions in a Crustal Anatectic Environment, Represented by Metapelitic Enclaves within El Hoyazo Dacites, SE Spain.Chemical Geology, 237:450-465. https://doi.org/10.1016/j.chemgeo.2006.07.014
    Bartoli, O., Acosta-Vigil, A., Ferrero, S., et al., 2016.Granitoid Magmas Preserved as Melt Inclusions in High-Grade Metamorphic Rock.American Mineralogist, 101(7):1543-1559. https://doi.org/10.2138/am-2016-5541ccbyncnd
    Bartoli, O., Cesare, B., Poli, S., et al., 2013a.Nanogranite Inclusions in Migmatitic Garnet:Behavior during Piston-Cylinder Remelting Experiments.Geofluids, 13(4):405-420. https://doi.org/10.1111/gfl.12038
    Bartoli, O., Cesare, B., Poli, S., et al., 2013b.Recovering the Composition of Melt and the Fluid Regime at the Onset of Crustal Anatexis and S-Type Granite Formation.Geology, 41(2):115-118. https://doi.org/10.1130/g33455.1
    Bartoli, O., Cesare, B., Remusat, L., et al., 2014.The H2O Content of Granite Embryos.Earth and Planetary Science Letters, 395:281-290. https://doi.org/10.1016/j.epsl.2014.03.031
    Bartoli, O., Tajmanová, L., Cesare, B., et al., 2013c.Phase Equilibria Constraints on Melting of Stromatic Migmatites from Ronda (S.Spain):Insights on the Formation of Peritectic Garnet.Journal of Metamorphic Geology, 31(7):775-789. https://doi.org/10.1111/jmg.12044
    Behrens, H., Roux, J., Neuville, D.R., et al., 2006.Quantification of Dissolved H2O in Silicate Glasses Using Confocal MicroRaman Spectroscopy.Chemical Geology, 229(1-3):96-112. https://doi.org/10.1016/j.chemgeo.2006.01.014
    Bodnar, R. J., Student, J. J., 2006. Melt Inclusions in Plutonic Rocks: Petrography and Microthermometry. In: Webster, J. D., ed., Melt Inclusions in Plutonic Rocks. Mineralogical Association of Canada, Montreal.
    Brown, M., 2002.Retrograde Processes in Migmatites and Granulites Revisited.Journal of Metamorphic Geology, 20(1):25-40. https://doi.org/10.1046/j.0263-4929.2001.00362.x