By Helmut G. F. Winkler (auth.), Edgar Froese (eds.)
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Additional info for Petrogenesis of Metamorphic Rocks
On the plane AI 20rFeO-MgO. Such minerals are chlorite, chloritoid, pyrophyllite, the modifications of AI 2SiO s, staurolite, cordierite, and almandine garnet considering only components almandine + pyrope and subtracting components grossularite, andradite, and spessartite from the chemical analysis. The K20-bearing minerals biotite and stilpnomelane plot inside the tetrahedron and muscovite (of ideal composition) and K feldspar are presented along the edge AI 20-K 20 of the tetrahedron. The tetrahedron AI 20rFeO-MgO-K 20 is shown in Figure 5-9.
253: 65-103. Wones, D. R. and Gilbert, M. C. 1969, Am. 1. Sci. 267 A: 480fl'. Yui, S. 1968. J. Mining Col. , Sel' A. 4: 29-39. Chapter 4 Mineral Parageneses: The Building Blocks of Metamorphic Rocks Rocks consist of a number of different minerals. In an igneous rock various minerals crystallized from a slowly cooling magmatic melt constitute an equilibrium assemblage. Such an assemblage is called a mineral paragenesis. In general, all the minerals that are detectable within a single thin section belong to the mineral paragenesis that characterizes a given igneous rock.
John Wiley & Sons, New York. Eugster, H. P. and Wones, D. R. 1962. 1. Petrol. 3: 82ff. Flinn, D. 1965. Deformation in metamorphism. In W. S. Pitscher and W. G. Flinn, eds. Controls oj Metamorphism. pp. 46-72. Oliver and Boyd, Edinburgh and London. French, B. M. 1966. Rev. Geophys. 4: 223-253. 26 Petrogenesis of Metamorphic Rocks Fyfe, W. , Turner, F. , and Verhoogen, 1. 1958. Geol. Soc. Am. Memoir 73. Griggs, D. T. and Blasic, J. D. Science 147: 292-295. Heard, H. C. 1. Geol. 71: 162-195. Jager, E.
Petrogenesis of Metamorphic Rocks by Helmut G. F. Winkler (auth.), Edgar Froese (eds.)