Geo Logica in collaboration with clastic sedimentation expert Deise Silveira from the Basin Analysis Research Lab (LABAP) at Federal University of Paraná (Brazil) is studying soft-sediment deformation and fluid escape features on the flanks of the Santa Cruz Diapir (Portugal).
Halokinesis is a process known to promote localised deformation of the sedimentary overburden deposited over and adjacent to salt structures (e.g., pillows, walls, diapirs).
In clastic settings where sediment consolidation rates are typically slow, bedding rotation induced by rapid diapir rise often involves soft-sediment deformation (SSD) and sediment rearrangement during flap development. Consequently, features such as slumps and deformation bands (e.g., granulation seams) are commonly observed, with increasing frequency near the salt diapir.
On the western flank of the Santa Cruz Diapir in the Lusitanian Basin (Portugal), Kimmeridgian-age deltaic fan units exhibit a steep upturned flap geometry. Along this flank, in addition to granulation seams and slumps, several SSD and fluid escape features, such as mega-scale convoluted bedding, and certain sand injectites cut through and intrude the sedimentary sequence. These structures are unevenly distributed along the flank.
Detailed sedimentological and structural fieldwork, complemented by UVA and LiDAR imagery interpretation, is being carried out on the western flank of the Santa Cruz Diapir to investigate the distribution and interrelationship of these structures and understand their origin and triggering mechanisms.
The fluid escape features can alter the permeability and connectivity of the reservoir, influence fluid migration, and affect the understanding of hydrocarbon distribution and storage, while playing a significant role in influencing stratigraphic and structural traps. The findings of this study highlight the importance of investigating and analysing these structures to improve the prediction of reservoir performance and hydrocarbon recovery strategies when modelling reservoirs and seals adjacent to salt diapirs.
These and other features associated with halokinesis are explained in our salt tectonics training course that will take place in October 2025. For more info about this course please visit our GeoTraining page: https://www.geologica.xyz/salt-tig-geo-logica-field-trip-i2