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By C. Aydinalp

ISBN-10: 9533078960

ISBN-13: 9789533078960

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The 48 An Introduction to the Study of Mineralogy estimated equilibration temperatures of the calcic amphiboles are presented in Table 4. Due to the absence of suitable coexisting mineral pairs, for the anthophyllite associated with the Sittampundi chromitites, we used the Plyusnina’s (1982) curve to calculate the equilibration temperature and found to range from 530-560oC. We have also used Graham & Powell’s (1984) hornblende-garnet geothermometry to calculate the equilibration temperature of the basic granulites.

Volcanic glass and allophanes are precursors to halloysite, which can also precipitate from the desilication of smectites (2:1 layer silicates) and may subsequently recrystallize to produce kaolinite (Allen and Hajek, 1989; Hendricks and Whittig, 1968; Southard and Southard, 1989). The absence of allophanes is related to the relative age of the soil. This soil, which is not glaciated and has been undergoing weathering for thousands of years, is presumably at an advanced stage of development that lies between the allophanic (or smectitic) and kaolinitic endmembers.

Tansley review no. 95 15N natural abundance in soil-plant systems. New Phytologist, 137: 179-203. F. M. 1986. Concentration of Iron Oxides from Soil Clays by Density Gradient Centrifugation. Soil Science Society of America Journal, 50: 1633-1639. Kendall, C. , 1998. Fundamentals of Isotope Geochemistry. In: Isotope Tracers in Catchment Hydrology (eds C. J. McDonnel), pp. 51-84. Elsevier Science, New York. A. O. 2003. Importance of mechanisms and processes of the stabilisation of soil organic matter for modelling carbon turnover.

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