Haselgebirge is a mylonite composed of mineral clay, sandstone, anhydrite, rock salt is and other salts.[1] The structure of the Hallstatt evaporite body (Northern 5 Calcareous Alps, Austria): a compressive diapir 6 superposed by strike-slip shear?
Haselgebirge is common is Alps, where it is used for salt extraction by the sinkworks method.
References
- ↑ "Structure and evolution of a rocksalt-mudrock-tectonite: The haselgebirge in the Northern Calcareous Alps", Journal of Structural Geology.
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