Combining shallow and deep geophysical information: the Yehuin–Chepelmut Fault Zone in the Magallanes fold and thrust belt (Tierra del Fuego, Argentina)

• Published in: International journal of earth sciences : Geologische Rundschau 2020-04, Vol.109 (3), p.971-994
• Main Authors: Lozano, Jorge G., Tassone, Alejandro, Bran, Donaldo M., Onnis, Luciano, Lodolo, Emanuele, Menichetti, Marco, Cerredo, María E., Esteban, Federico, Ormazabal, Juan P., Ísola, José, Baradello, Luca, Vilas, Juan F.
• Format: Article
• Language: English
• Subjects: Basins; Cretaceous; Deformation; Earth and Environmental Science; Earth Sciences; Electrical resistivity; Fault lines; Fault zones; Geochemistry; Geological faults; Geology; Geophysical surveys; Geophysics; Geophysics/Geodesy; Glaciers; Magnetic measurement; Mineral Resources; Neogene; Original Paper; Outcrops; Sedimentology; Seismic analysis; Seismic surveys; Stress distribution; Structural Geology; Tomography
• ISSN: 1437-3254; 1437-3262
• DOI: 10.1007/s00531-020-01847-3

The outer Fuegian fold and thrust belt is the deformed sector of the Austral-Magallanes Basin, which underwent a contractional phase since the Late Cretaceous and a strike-slip phase during the Neogene. The area hosts two Neogene basins (Yehuin and Chepelmut) which have been mainly developed by the influence of wrench deformation, and were subsequently modified by glacial activity of the Ewan and Fuego glacier lobes of the Fagnano palaeoglacier. Geophysical surveys using Electrical Resistivity Tomography, onland shallow seismic surveys, and magnetometry, have been combined with outcrop analysis and deep seismic lines to recognize both shallow and intermediate deep structures related to the lacustrine basins. Four sets of faults with different deformation history were involved in the basin genesis. Comparison with the Deseado Fault Zone indicates similarities of the structural features between the two zones. The stress field interpreted as responsible for the origin of the studied basins is analogous to the one in the Deseado valley, located in the western Tierra del Fuego. Therefore, a transcurrent fault zone, here named Yehuin–Chepelmut Fault Zone, is proposed as part of the diffuse boundary between South America and Scotia plates.