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https://doi.org/10.2113/gssgfbull.s5-xv.7-8.453
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Cite Publication Date: Jan 1, 1945 | |
 Citations: 3 |
Abstract Describes cone-in-cone structures from middle Arenig (Ordovician) deposits of the Montagne Noire, France, and concludes that the structures are organic concretions which later were subjected to lateral pressures, not necessarily of tectonic origin.
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