Monoklint

Monoklint is a term used in geology to describe a fold in rock strata where the dip of the layers on both sides of the fold is in the same direction. This is in contrast to a syncline or anticline, where the dip is towards or away from the fold axis, respectively. Monoklinal folds are characterized by a relatively uniform dip angle across the fold.

These structures can form through various tectonic processes. They are often found in areas experiencing compressional forces, but can also develop under extensional or shearing regimes. The specific geometry of a monoklint depends on factors such as the rock type, the magnitude and direction of the applied stress, and the existing geological structure. Monoklinal folds can occur as single features or as part of larger, more complex fold systems.

In sedimentary basins, monoklinal structures can influence the distribution of hydrocarbons, as they can create traps for oil and gas. Geologists study monoklints to understand the deformation history of a region and to aid in resource exploration. The term is less commonly used than anticline or syncline, but it provides a specific description for this particular fold geometry.