Abstract
The central Andes is part of a Cordilleran orogen formed through continent-ocean convergence. In contrast to the thickened crust, the mantle lithosphere below much of the orogen is anomalously thin. Additionally, the surface is characterized by widespread backarc magmatism and transient ∼100-km-wide basins that developed the over last 30 million years, with basins located systematically seaward of major backarc ignimbrite centers and basin formation predating the late Miocene magma/ignimbrite flare-up. Using numerical models, we propose a novel mechanism whereby lithosphere removal is coupled with mantle flow. First, a small area of high-density eclogitized lower crust initiates a gravitational instability, causing a localized basin at the surface that subsides and then uplifts. Foundering crust and adjacent lithosphere are entrained by subduction-induced mantle flow, driving regional lithosphere removal and magmatism. The models demonstrate that mantle flow can amplify a local lithosphere instability to orogen-wide lithosphere removal, rapidly eliminating accumulated mass in the orogen.
Original language | English (US) |
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Article number | e2021GL095075 |
Journal | Geophysical Research Letters |
Volume | 48 |
Issue number | 16 |
DOIs | |
State | Published - Sep 16 2021 |
Keywords
- Andean subduction
- hinterland basins
- ignimbrite magmatism
- lithosphere removal
- mantle flow
ASJC Scopus subject areas
- Geophysics
- General Earth and Planetary Sciences