F. Boudinage

Figure 1. Boudinage. Top: boudins; bottom: chocolate tablet structure.


Buckle folds are formed when strong (or ‘‘) layers of rock are shortened. What happens when strong layers are extended? Typically the layers start to thin at points of weakness (a process known in engineering as ) producing a structure called pinch-and-swell. As pinch and swell develops, the thin regions can separate, leaving a structure that looks like a string of sausages in cross-section. The remnants of the original layer are called (a French word for a type of sausage), and the process is known as .

Although boudins are in many ways the extensional counterpart of folds, the terminology of boudinage is much less well developed than that of folds. In part, this is because layers undergoing boudinage do not affect adjacent layers in the same way, so that boudins are less likely to be harmonic than folds. Thus, although boudins do have axes, it is rarely possible to define an equivalent of an axial surface for boudins.

Sometimes layers undergo extension in all directions simultaneously, producing a more three-dimensional boudinage structure described as . It is also possible to find examples of layers that have undergone both folding and boudinage during progressive deformation.

Figure 2. Boudins formed from quartz vein. Carmanville, Newfoundland.


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Geological Structures: a Practical Introduction by John Waldron and Morgan Snyder is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License, except where otherwise noted.

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