Structural features of the southern Tulum Fault System, western central Argentina, through gravimetric data and geomorphologic analyses

• The Tulum Fault System corresponds to basement blocks uplifts of a broken foreland basin system.
• Two depocenters that would be flexural foreland basins were recognized and were called “El Cerro” and “Barboza” depocenters.
• Depocenters can be recognized as the foredeep and backbulge depozones and between them a forebulge depozone.

A gravimetric analysis over the Tulum Valley was made. This data was used to reveal the structural setting of the Tulum Fault System situated in the southeastern part of San Juan province in the arid western part of Argentina. This system is the boundary between two geological provinces, the eastern Precordillera Oriental and the Sierras Pampeanas Occidentales. Gravity data was processed using upward continuation and vertical derivative filters and all the results were compared with the geomorphological and the drainage systems maps of the area. Our assessment confirms the presence of two structures in the Pampeano basement with positive anomalies similar to those found in Valdivia and Barboza hills, two important depocenters with low gravimetric gradients separated by a zone with higher gravity anomalies than the depocenters to the east and west. In view of this, a structural map is proposed for the area. This system is important not only because it is the boundary between two geological provinces and has significance regarding regional tectonic issues but also because it controls the surface drainage, soils distribution and groundwater flow of the Tulum basin conditioning the land use distribution.