Absolute Age and Temperature Constraints on Deformation Along the Basal Décollement of the Jura Fold‐and‐Thrust Belt From Carbonate U‐Pb Dating and Clumped Isotopes. Issue 3 (17th March 2021)

• Record Type: Journal Article
• Authors: Looser, N.; Madritsch, H.; Guillong, M.; Laurent, O.; Wohlwend, S.; Bernasconi, S. M.
• Is Part Of: Tectonics. Volume 40:Issue 3(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-03-17
• Subjects: basal décollement -- carbonate U‐Pb dating -- clumped isotope thermometry -- deformation timing -- fold‐and‐thrust belt -- Jura Mountains; Geology, Structural -- Periodicals; 551.8
• DOI: 10.1029/2020TC006439
• Languages: English
• ISSNs: 0278-7407

Abstract

Abstract: During its late‐stage evolution, the European Alpine orogen witnessed a northwest‐directed propagation of its deformation front along an evaporitic basal décollement into the foreland. This resulted in the decoupling of the northern Alpine Molasse Basin from its basement and the formation of the Jura fold‐and‐thrust belt. Here, we present the first absolute age and temperature constraints on deformation along this basal décollement using carbonate U‐Pb LA‐ICP‐MS dating and clumped isotope thermometry. We analyzed calcite veins associated with a thrust fault branching off from the basal décollement in the distal Molasse Basin and slickenfibers from thrusts and strike‐slip faults in the eastern Jura Mountains. Our U‐Pb data provide evidence for tectonic activity related to Alpine contraction between 14.3 and 4.5 Ma ago. According to the oldest deformation ages, the propagation of Alpine deformation into the distal foreland along the basal décollement occurred earlier than previously inferred by biostratigraphy, at Middle Miocene (Langhian) times at the latest. Younger deformation ages between 11.3 and 4.5 Ma correspond very well in time with shortening in the Subalpine Molasse and the Central Alps, proving simultaneous tectonic activity along both thrust fronts; i.e., the Jura Mountains and the Subalpine Molasse. Clumped isotopes reveal vein calcite precipitation at temperatures between 53 and 104 °C from fluids with oxygen isotope compositions between −6.2‰ and +9.5‰ reflecting distinct burial settings. Combined, our U‐Pb and clumped isotope data show that the burial conditions in the studied area remained constant between 14.3 and 4.5 Ma indicating that large‐scale foreland erosion did not initiate before 4.5 Ma. Key Points: Propagation of Alpine deformation along the basal décollement into the distal foreland initiated at 14.3 Ma at the latest Deformation occurred over a time period of at least ∼10 Ma (14.3–4.5 Ma) with contemporaneous activity of thrusts and strike‐slip faults Constant in situ temperatures and fluid sources show that large‐scale foreland erosion did not initiate before 4.5 Ma