Demystifying migmatites: introduction for field-based geologist

作者: M. Pawley , A. Reid , R. Dutch , W. Preiss

DOI: 10.1179/1743275815Y.0000000014

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摘要: Migmatites are heterogeneous, medium- to high-grade metamorphic rocks with at least one component formed by partial melting. As migmatites form under P–T conditions common in the middle and lower crust, they widespread likely be encountered field. They complex that can confusing, present paper provides a background for field-based geologist. comprise several main components. Neosome is newly melting includes leucosome residuum (or melanosome). These essentially represent liquid solid components of melt reaction. Palaeosome part migmatite did not undergo typically more refractory composition. divided into two types. Metatexites have fraction preserve coherent pre-partial textures palaeosome. Diatexites dominated neosome, structures absent. further subdivid...

参考文章(68)
R. W. WHITE, R. POWELL, J. A. HALPIN, Spatially-focussed melt formation in aluminous metapelites from Broken Hill, Australia Journal of Metamorphic Geology. ,vol. 22, pp. 825- 845 ,(2005) , 10.1111/J.1525-1314.2004.00553.X
R. W. WHITE, N. E. POMROY, R. POWELL, An in situ metatexite–diatexite transition in upper amphibolite facies rocks from Broken Hill, Australia Journal of Metamorphic Geology. ,vol. 23, pp. 579- 602 ,(2005) , 10.1111/J.1525-1314.2005.00597.X
R. W. White, R. Powell, T. J. B. Holland, Calculation of partial melting equilibria in the system Na2O–CaO–K2O–FeO–MgO–Al2O3–SiO2–H2O (NCKFMASH) Journal of Metamorphic Geology. ,vol. 19, pp. 139- 153 ,(2008) , 10.1046/J.0263-4929.2000.00303.X
R. W. White, R. Powell, Melt loss and the preservation of granulite facies mineral assemblages Journal of Metamorphic Geology. ,vol. 20, pp. 621- 632 ,(2002) , 10.1046/J.1525-1314.2002.00206.X
I. van der Molen, M. S. Paterson, Experimental deformation of partially-melted granite Contributions to Mineralogy and Petrology. ,vol. 70, pp. 299- 318 ,(1979) , 10.1007/BF00375359
A. Dana Johnston, Alberto E. Pati�o Douce, Phase equilibria and melt productivity in the pelitic system: implications for the origin of peraluminous granitoids and aluminous granulites Contributions to Mineralogy and Petrology. ,vol. 107, pp. 202- 218 ,(1991) , 10.1007/BF00310707