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doi: 10.1038/061612a0
IF the intercrossing of two separate systems of folding be the essential condition in the complicated rock-structures so ably worked out by Mrs. M. M. Ogilvie Gordon in South Tyrol, I scarcely think the parallelism with the conditions in the Manx Carboniferous rocks can be so close as Mrs. Gordon suggests in her recent letter (NATURE, March 22, p. 490).
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