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The Middle Badenian anhydrite sections in the central part of the Carpathian Foredeep consist mainly of interbedded laminated anhydrite and anhydrite breccia. These facies display features characteristic of redeposited sediments such as distortions due to slumping, erosional boundaries, and graded-bedded laminae. Lamination in laminated anhydrite is rarely regular and often accompanied by disruptions...
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