Abstract
DTA curves of natural dolomites of various origins were recorded under identical experimental conditions. Variations in Te.o. and peak shape of the first endotherm are considered in relation to chemical composition, structural deviation from ideal dolomite and sieve and true grain size.
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References
T. L. Webt and J. E. KrĂĽger, Differential Thermal Analysis (ed. R. C. Mackenzie), Vol. 1, Academic Press, London (1970) Chap. 10, 303
J. L. Kulp, P. Kent, and P. K. Kerr, Am. Mineral. 36 (1951) 643
R. I. Harker and O. E. Tuttle, Am. J. Sci. 253 (1955) 274
J. R. Goldsmith and D. L. Graf, J. Geol. 66 (1958) 678
W. Smykatz-KLoss, Contr. Mineral. Petro. 13 (1966) 207
R. C. Mackenzie and B. D. Mitchell, Thermal Investigation of Clays, Min. Soc, London (1957) Chap. II, 23
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© 1980 Springer Basel AG
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Otsuka, R., Tanabe, S., Iwafuchi, K., Ozao, R. (1980). DTA Curves of Dolomites of Various Origins. In: Hemminger, W. (eds) Thermal Analysis. Birkhäuser, Basel. https://doi.org/10.1007/978-3-0348-6736-8_46
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DOI: https://doi.org/10.1007/978-3-0348-6736-8_46
Publisher Name: Birkhäuser, Basel
Print ISBN: 978-3-0348-6737-5
Online ISBN: 978-3-0348-6736-8
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