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In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved ("folded") during permanent deformation. Folds in rocks vary in size from microscopic crinkles to mountain-sized folds. They occur as single isolated folds or in periodic sets (known as fold trains).
Therefore, the number of 2-, 3-, 4-, and 6-fold rotocenters per primitive cell is 4, 3, 2, and 1, respectively, again including 4-fold as a special case of 2-fold, etc. 3-fold rotational symmetry at one point and 2-fold at another one (or ditto in 3D with respect to parallel axes) implies rotation group p6, i.e. double translational symmetry ...
The vergence of a fold can help a geologist determine several characteristics of folding on a larger scale, including the style, position, and geometry of the folding. [ 3 ] By observing vergence in a fold, geologists can record data that can be used to calculate the approximate position and geometry of a larger area, and therefore assist ...
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Four circles meet at each vertex. Each circle represents axes of 3-fold symmetry. The 600-cell edges projected onto a 3-sphere represent 72 great circles of H4 symmetry. Six circles meet at each vertex. Each circle represent axes of 5-fold symmetry. Direct subgroups of the reflective 4-dimensional point groups are:
English: An idealized thrust fault with a fault-propagation fold. Diagram to clearify terminology in structural geology. Diagram to clearify terminology in structural geology. Sources for this diagram:
The two groups are obtained from it by changing 2-fold rotational symmetry to 4-fold, and adding 5-fold symmetry, respectively. There are two crystallographic point groups with the property that no crystallographic point group has it as proper subgroup: O h and D 6h. Their maximal common subgroups, depending on orientation, are D 3d and D 2h.
The 3-fold axes are now S 6 (3) axes, and there is a central inversion symmetry. T h is isomorphic to T × Z 2 : every element of T h is either an element of T, or one combined with inversion. Apart from these two normal subgroups, there is also a normal subgroup D 2h (that of a cuboid ), of type Dih 2 × Z 2 = Z 2 × Z 2 × Z 2 .
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