By S. Ghose, J. Ganguly (auth.), Surendra K. Saxena (eds.)
The moment quantity of this sequence contains 3 components. half I makes a speciality of the learn on intracrystalline reactions. This paintings, which all started approximately 20 years in the past, is severely reviewed by means of Ghose and Ganguly in bankruptcy 1. in addition to the evaluation, the authors comprise a few of their formerly unpublished paintings to illustrate how destiny learn may well relief in acquiring information on thermodynamics of stable recommendations and in figuring out the cooling background of igneous and metamorphic rocks. The latter can be the subject followed by way of Kretz within the moment bankruptcy, which examines the redistribution of Fe and Mg in coexisting silicates in the course of cooling. bankruptcy three includes new information on Fe-Mg distribution in clinopyroxenes. Dal Negro and his co-authors have chosen a chain of clinopyroxenes from volcanic rocks and current web site occupancy facts on numerous clinopyroxenes of intermediate compositions. the knowledge set has now not been released earlier than and is the 1st of its sort. half II of this ebook starts off with a bankruptcy on melts by means of Gaskell, who explores the connection among density and constitution of silicate melts. this is often through the synthesis of knowledge generated within the U.S.S.R. via Shmulovich and his co-authors on fluids. Blencoe, Merkel and Seil current a radical research of the section equilibrium information on feldspars coexisting with fluids within the 3rd bankruptcy during this part.
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63, 1053-1073. Veblen, D. , Buseck, P. , and Burnham, C. W. (1977) Asbestiform chain silicates: new minerals and structural groups, Science 198, 359-365. , and Hafner, S. (1969) Fe2+, Mg order-disorder in heated orthopyroxenes, Mineral. Soc. Amer. Spec. Pap. 2, 67-81. , and Hafner, S. S. (1972) Temperature-dependent Mg, Fe distribution in a lunar olivine, Earth. Planet. Sci. Lett. 14, 305-312. , and Ghose, S. (1965) The effect of Mg2+ _Fe2+ substitution on the cell dimension of cummingtonites, Amer.
Splitting of the fundamental O-H stretching band in cummingtonites (after Burns and Strens, 1966). Table 16. Comparison of site occupancies determined by single crystal X-ray diffraction and infra-red spectroscopy in a grunerite. 92 aFinger (1969). bBurns and Strens (1966). ble. The accuracy and precision of the site occupancy determination from ir spectra is difficult to evaluate. The comparison of the site occupancies in a grunerite determined by single crystal X-ray diffraction and ir techniques is shown in Table 16.
And Ganiel, U. (1967) Mossbauer studies of Fe2+ in paramagnetic fayalite (Fe2Si04). Solid State Commun. 5, 267-270. Evans, B. , and Hafner, S. (1967) Hyperfine splitting of Fe57 and Mg-Fe order-disorder in orthopyroxenes (MgSi0 3 solid solution). J. Geol. 75, 306-322. Evans, B. , Rice, J. , and Trommsdorff, V. (1974) Cummingtoniteanthophyllite phase transformation in metamorphosed ultramafic rocks, Ticino, Switzerland. Trans. Am. Geophys. Union 55, 469. Finger, L. W. (1969) The crystal structure and cation distribution of a grunerite.