imbricate

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The folds observed in the imbricates of Silurian and Devonian rocks could have different origins.
Thrusts form an imbricate fan system with numerous imbrications of Silurian black shales and Siluro-Devonian limestones (Figs.
In the western limb of the synclinorium, normal faults, approximately parallel to the trend of the limb, are superimposed on the imbricate structure of Silurian and Devonian units.