Abstract
ALBITE-oligoclase feldspar concentrations occur abundantly in the Eocambrian to Lower Ordovician metasediments, along the entire metamorphic Caledonian–Appalachian mountain chain. In Spitsbergen (refs. 1 and 2 and personal communication from W. Horsfield); Stavanger, Norway; SE Scotland; Antrim, N. Ireland; Co. Mayo, Ireland3; Burlington Peninsula, Newfoundland; Pennsylvania; Dutchess County, New York4; and Maryland, particular attention has been given to the albite schist association.
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Harland, W. B., Wallis, R. M., and Gayer, R. A., Geol. Mag., 103, 70 (1966).
Wallis, R. H., Norsk Polarinstitutt, 80, 108 (1969).
Kennedy, M. J., Proc. Roy. Irish Acad., 66B, 261 (1969).
Knopf, E. B., and Jones, A. I., US Geol. Survey, B 799, 1 (1929).
Singlewald, J. T., Brit. Geol. Soc. Amer., 43, 449 (1932).
Degens, E. T., and Ross, D. A., Hot Brines and Recent Heavy Metal Deposits in the Red Sea (Springer-Verlag, New York, 1969).
Hay, R. L., Geol. Soc. Amer., special paper 85 (1966).
Pautot, G., Auzende, J. M., and LePichon, X., Nature, 227, 351 (1970).
Dewey, J. F., and Bird, J. M., J. Geophys. Res., 75 (in the press).
Wilson, J. T., Nature, 211, 676 (1966).
Bird, J. M., and Dewey, J. F., Bull. Geol. Soc. Amer., 81, 1031 (1970).
McKenzie, D. P., and Parker, R. L., Nature, 216, 1276 (1967).
Schaub, H. P., Med. om. Gronland, 114(ID), 1 (1950).
Borchert, M., and Muir, R. O., Salt Deposits, the Origin, Metamorphism and Deformation of Evaporites (van Norstrand, 1964).
Engel, A. C. J., and Engel, C. G., Bull. Geol. Soc. Amer., 64, 1013 (1953).
Shaw, D. M., J. Petrol., 1, 218 (1960).
Orville, P. M., Norsk Geologish Tidsskrift, 42 B, 281.
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WIT, M. Evidence for Salt Deposits in the Appalachian/Caledonian Orogen. Nature 227, 829–830 (1970). https://doi.org/10.1038/227829b0
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DOI: https://doi.org/10.1038/227829b0
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