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Regional variation in the crustal abundance of minor elements: evidence from the granites of Sardinia

Published online by Cambridge University Press:  05 July 2018

A. Hall
A. Hall*
Affiliation:
Department of Geology, King's College, Strand, London, WC2R 2LS
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Summary

The granites of Sardinia have been analysed for copper, lead, and zinc, and each element has been found to show a regional variation. There is a close relationship between the copper and lead contents of the granites and the distribution of copper and lead mineralization in the island, but very little relation between the zinc contents of the granites and the distribution of zinc mineralization. This is attributed to a greater degree of lithophile character of zinc in the magmatic source region.

Type
Research Article
Information
Mineralogical Magazine , Volume 40 , Issue 311 , September 1975 , pp. 293 - 301
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1975

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References

Albuquerque, (C. A. R. de), 1971. Bull. Geol. Soc. Amer. 82, 2783-98.CrossRefGoogle Scholar
Coats, (J. S.) and Wilson, (J. R.), 1971. Min. Mag. 38, 138-51.CrossRefGoogle Scholar
Dee Mort, (A.), DI Simplicio, (P.), and Rita, (F.), 1972. Min. Petr. Acta, 18, 245-54.Google Scholar
Dodge, (F. C. W.), 1972. Bull. U.S. Geol. Surv. 1314-F, 13 pp.Google Scholar
Flinter, (B. H.), Hesp, (W. R.), and Rigbv, (D.), 1972. Econ. Geol. 67, 1241-62.CrossRefGoogle Scholar
Garrett, (R. G.), 1972. In Geochemical Exploration 1972, pp. 203-19, London (Institution of Mining and Metallurgy).Google Scholar
Ghezzo, (C.), Guasparri, (G.), and Sabatini, (G.), 1972. Min. Petr. Acta, 18, 205-34.Google Scholar
Hall, (A.), 1973a. Geol. Mag. 110, 467-72.CrossRefGoogle Scholar
Hall, (A.), 1973b. Nature (Phys. Sci.), 242, 72-5.CrossRefGoogle Scholar
Kolbe, (P.) and Taylor, (S. R.), 1966. Contr. Min. Petr. 12, 202-22.CrossRefGoogle Scholar
Manrei, (E.), Bolrer, (E.), and Al Shaieb, (Z.), 1970. Min. Deposita, 5, 184-90.Google Scholar
O'leary, (M.), Lippert, (R. H.), and Spitz, (O. T.), 1966. Computer Contrib. Kansas Geol. Surv., 3, 48.pp.Google Scholar
Smith, (F. G.), 1963. Physical Geochemistry. Reading, Mass. (Addison-Wesley).Google Scholar
Snedecop, (G. W.) and Cocaran, (W. G.), 1967. Statistical Methods. Ames, Iowa (Iowa State University Press).Google Scholar
Turekian, (K. K.) and Wedepohl, (K. H.), 1961. Bull. Geol. Soc. Amer. 72, 175-92.CrossRefGoogle Scholar
Zlobin, (B. I.), Pevtsova, (L. A.), and Klassova, (N. S.) [ЗɅOбиH, (Б. И.), ПeBцOBa, (Ʌ. A.), и КʌaccoBa, (H. C.)] 1965. Geochem. Internat. 2, 660-71.(transl. of ГeoxиMия)Google Scholar
Zuffardi, (P.), 1965. Boll. Assoc. Mineraria Subalpina, 2, no. 2, 1–42.Google Scholar
Zuffardi, (P.), 1969. Ann. Soc. géol. Belgique, 92, 321-44.Google Scholar