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Fourmarier's Suction Theory of Geosynclines, and the ``Vertical Push'' Explanation of Geanticlinal Orogeny

C. A. Cotton
Science
New Series, Vol. 116, No. 3010 (Sep. 5, 1952), p. 261
Stable URL: http://www.jstor.org/stable/1680885
Page Count: 1
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