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A salt dome is a type of structural dome formed when salt (or other evaporite minerals) intrudes into overlying rocks in a process known as diapirism. Salt domes can have unique surface and subsurface structures, and they can be discovered using techniques such as seismic reflection .
Excavated salt domes are also used for underground storage. Diapirs or piercement structures are structures resulting from the penetration of overlaying material. By pushing upward and piercing overlying rock layers, diapirs can form anticlines (arch-like shape folds ), salt domes (mushroom/ dome-shaped diapirs), and other structures capable of ...
Saldome 1 and 2 are two very large wooden cupola buildings near Möhlin, SwitzerlandThey both serve to store the Swiss stockpile of road de-icing salt.At the time of construction, Saldome 2 was the largest wooden dome of Europe.
Salt surface structures are extensions of salt tectonics that form at the Earth's surface when either diapirs or salt sheets pierce through the overlying strata. They can occur in any location where there are salt deposits, namely in cratonic basins, synrift basins, passive margins and collisional margins .
The Schacht Asse II and Gorleben salt domes in Germany are an example of a purely passive salt structure. [citation needed] Such structures do not always form when a salt layer is buried beneath a sedimentary overburden.
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