Lower-middle ordovician sedimentary environment and provenance of the suri formation in the northern region of the Famatina belt, Catamarca, Argentina.

The Suri Formation is a sedimentary-volcanic succession in the Famatina belt formed during Lower - Middle Ordovician arc magmatism along the western margin of Gondwana. This study reports new lithostratigrafic data relating to the Suri Formation in the Chaschuil valley (Catamarca). The survey defines the main characteristics of volcanism and sedimentation through facies analysis. Epiclastic, volcaniclastic, pyroclastic and peperitic facies were recognized and interpreted in five facies association. The features and relationships of the facies associations indicate environments such as apron volcaniclastic, inner to an outer shelf, and fan distal delta, interbedded with effusive and explosive volcanism. Volcanic activity and relative sea-level changes were controls on sedimentation style in basins adjacent to the volcanic edifice. The study reports U–Pb geochronological analysis of zircon from a sandstone sample of the Suri Formation to infer detrital provenance. The detrital zircon pattern with peaks at 486 Ma points to active Famatinian magmatism as recorded on the nearby Narváez batholith. Eruptive masses experienced rapid reworking, short sedimentary transport and intra-arc deposition. The maximum deposition age of detrital zircon corresponds to a subordinate age cluster at 464.4 ± 4.4 Ma and reflects synchronism between volcano-sedimentary deposition in the Suri Formation and plutonic-volcanic construction of the Las Planchadas Formation. • This study reports a stratigraphic analysis of the Suri Formation in the northern Famatina System. • The Suri Formation reflects apron volcaniclastic, internal to external shelf and fan distal delta. • Variable intensity of volcanism controlled the sedimentary environment of Suri Formation. • Volcanic facies contain abundant proximal deposits suggestive of explosive eruptive activity. • Sedimentation of the Suri Formation reveals a topographic surface with high slope gradient. [ABSTRACT FROM AUTHOR]