Dikesdragningar
Dikesdragningar is a term used in geology, particularly in Swedish-language literature, to describe the study and documentation of igneous dike intrusions that cut across pre-existing rock formations. Dikes are tabular or sheet-like bodies of igneous rock that crystallized from magma propagating through fractures in the crust. The practice of dikesdragningar involves mapping the occurrence, orientation, thickness, and cross-cutting relationships of these dikes to reconstruct magmatic episodes and the tectonic history of a region.
In dikesdragningar, field work focuses on recording the strike and dip of dikes, their spatial distribution,
The information gathered through dikesdragningar contributes to broader geological understanding, including crustal structure, tectonic evolution, and