This review paper examines deformation adjacent to salt stocks and walls and beneath salt
sheets, with a focus on passive salt rise or emplacement and structures ranging from large …

This work aims to present the Les Avellanes diapir as a field analog to inquire how the
origin, advance, and emplacement of an allochthonous salt body in continental settings …

Halokinetic deformations synchronous with salt deposition are processes already suggested
in several salt giants including the Lower Cretaceous salt deposits of the Santos Basin in …

This contribution describes the influence of diapirism and compressional tectonics in the
sedimentary record of the Estopanyà and Boix synclines (salt-walled basins) in the South …

Inherited and syn-compressional salt-controlled structures in orogens are difficult to
distinguish from compressional features because classical salt features (halokinetic growth …

The 1 km thick evaporitic Permian Zechstein group in the Netherlands is subdivided into 5
halite rich evaporitic sequences including K–Mg salts (polyhalite, kieserite, sylvite, carnallite …

Stratal geometries of salt-floored minibasins provide a record of the interplay between
minibasin subsidence and sedimentation. Minibasin subsidence and resulting stratal …

Salt–sediment interaction during passive diapirism typically occurs at two distinct scales that
are related to depositional relief from the highs above diapirs to the lows of adjacent …

The EW oriented Sivas foreland basin in Turkey recorded a salinity crisis during the Late
Eocene resulting in evaporite accumulations thick enough to trigger intense halokinesis …

Abstract The Sivas Basin is located in the eastern part of the central Anatolia. In this study,
aeromagnetic data in the basin and surrounding area are processed and anomalies are …