ABABStapelung

ABABStapelung is a term used in the field of geology and structural geology to describe a specific type of folding in sedimentary rocks. The term is derived from the German words "A" for anticline and "B" for syncline, with "Stapelung" meaning "stacking" or "piling up". The ABABStapelung structure is characterized by a series of alternating anticlines and synclines, stacked one above the other, which results in a distinctive pattern of folding.

This type of folding is often associated with the deformation of sedimentary sequences due to tectonic forces. The anticlines and synclines are typically symmetrical and have similar wavelengths, which contributes to the regular stacking pattern. The ABABStapelung structure can provide valuable insights into the geological history of a region, as it reflects the sequence of tectonic events and the nature of the stresses that acted upon the rocks.

The term ABABStapelung was first introduced by the German geologist Karl Alfred von Zittel in the late 19th century. Since then, it has been widely used in the geological literature to describe similar folding patterns in various sedimentary basins around the world. The study of ABABStapelung structures is an important aspect of structural geology, as it helps to understand the complex processes involved in the deformation of the Earth's crust.