Rotation of crustal domains related to Gondwanide deformation in the Neoproterozoic–Cambrian Sauce Chico Complex (Argentina), southwestern margin of the Río de la Plata Craton: Insights from AMS data

VAZQUEZ LUCERO, S.E.; BALLIVIÁN JUSTINIANO, C.A.; FAZZITO, S.; PREZZI, C.B.; RUÍZ GONZÁLEZ, V.; RODRÍGUEZ, S.; VIZÁN, H.

PRECAMBRIAN RESEARCH

ELSEVIER SCIENCE BV

Año: 2024 vol. 406

0301-9268

The tectonic evolution of the Ventania System fold and thrust belt and the origin of its curvature have been thesubject of debates for decades. The Gondwanide Orogeny generated the mylonitization of its Tonian–middleCambrian basement (i.e., Sauce Chico Complex), accompanied by an intense hydrolysis which produced secondarymuscovite (i.e., sericite), and the folding of the overlying Paleozoic sedimentary cover. To evaluate thestructural and tectonic evolution of the Ventania System as a result of the interaction of its basement with the Ríode la Plata Craton, we studied the anisotropy of magnetic susceptibility (AMS) and rock magnetism on samples ofthe Sauce Chico Complex. Rock magnetic studies suggest that paramagnetic minerals are the main carriers in theentire Sauce Chico Complex. We suggest that our results reflect secondary muscovite generation due to mylonitization.AMS data reveal that the orientation of the magnetic foliation coincides to a large extent with the rockfoliation. However, magnetic and rock foliation orientations are not uniform among the different sampled units,displaying strikes between N 320◦ (NW) and N 345◦ (NNW) on average. Localities with different orientations areseparated by regional strike-slip structures, referred to as tear faults, which have also been reported and interpretedby previous authors. According to this, we suggest that the variations detected between the orientation ofthe magnetic and rock foliations of the different basement units may be the result of the rotation of crustal blocksbounded by tear faults. We also propose the existence of a new tear fault not previously recognized. Furthermore,a tear fault of regional character, known as the Sauce Chico Tear Fault, juxtaposes two distinct crustal domains.The differential displacement of such domains could have contributed not only to different structural stylesbetween blocks on both sides of the Sauce Chico Tear Fault, but also to the curved shape of the Ventania Systemduring the progression of the Gondwanide deformation.