Kinematics, Exhumation, and Sedimentation of the North Central Andes (Bolivia): An Integrated Thermochronometer and Thermokinematic Modeling Approach. Issue 11 (16th November 2017)

• Record Type: Journal Article
• Authors: Rak, Adam J.; McQuarrie, Nadine; Ehlers, Todd A.
• Is Part Of: Tectonics. Volume 36:Issue 11(2017)
• Page Start: 2524
• Page End: 2554
• Publication Date: 2017-11-16
• Subjects: thermochronometer -- thermokinematic -- Andes -- Bolivia -- isostasy -- sedimentation; Geology, Structural -- Periodicals; 551.8
• DOI: 10.1002/2016TC004440
• Languages: English
• ISSNs: 0278-7407

Abstract

Abstract: Quantifying mountain building processes in convergent orogens requires determination of the timing and rate of deformation in the overriding plate. In the central Andes, large discrepancies in both timing and rate of deformation prevent evaluating the shortening history in light of internal or external forcing factors. Geologic map patterns, age and location of reset thermochronometer systems, and synorogenic sediment distribution are all a function of the geometry, kinematics, and rate of deformation in a fold‐thrust‐belt‐foreland basin (FTB‐FB) system. To determine the timing and rate of deformation in the northern Bolivian Andes, we link thermokinematic modeling to a sequentially forward modeled, balanced cross section isostatically accounting for thrust loads and erosion. Displacement vectors, in 10 km increments, are assigned variable ages to create velocity fields in a thermokinematic model for predicting thermochronometer ages. We match both the pattern of predicted cooling ages with the across strike pattern of measured zircon fission track, apatite fission track, and apatite (U‐Th)/He cooling ages as well as the modeled age of FB formations to published sedimentary sections. Results indicate that northern Bolivian FTB deformation started at 50 Ma and may have begun as early as 55 Ma. Acceptable rates of shortening permit either a constant rate of shortening (~4–5 mm/yr) or varying shortening rates with faster rates (7–10 mm/yr) at 45–50 Ma and 12–8 Ma, significantly slower rates (2–4 mm/yr) from 35 to 15 Ma and indicate the northern Bolivian Subandes started deforming between 19 and 14 Ma. Key Points: Isostatically compensated, balanced cross section linked to a thermokinematic model Basement thrust sheets set the first‐order cooling pattern that matches measured ages in Bolivian Andes FTB deformation started at 50 Ma with peak shortening at ~50–45 Ma and ~12–8 Ma