Work

Hydration weakening and destruction of the North China Craton

Year: 2025

Type: article

Abstract: Cratons are generally considered the most stable parts of the lithosphere. However, recent studies have shown that some cratons have undergone significant thinning and even destruction. The destruction of the eastern part of the North China Craton has been documented through numerous geological, geochemical, and geophysical investigations. Yet, the exact mechanism behind this extensive thinning remains a subject of debate. In this study, we develop two dimensional (2-D) box models in a finite difference code LaMEM to identify the most viable reasons for the destruction of the North China Craton (NCC). We examine the role of slab-induced hydration, high-density lower crust, and weak mid-lithospheric discontinuity in our models. Results indicate that a low angle or flat slab-induced hydration weakening of the eastern part of the NCC can lead to rapid craton destruction if hydration weakening rates are sufficiently fast. This accelerated hydration rate may be attributed to the extensive carbonatite magmatism within the eastern part of the NCC, facilitating a faster pathway for water diffusion throughout the craton. Rapid craton destruction is also contingent upon the craton's density exceeding the surrounding mantle density, and its viscosity decreasing below 10 22 Pa s. We observe that the presence of a dense lower crust or a mid-lithospheric discontinuity fail to destroy the NCC unless the craton is sufficiently weakened. • 2D thermo-mechanical modeling to investigate the destruction of the eastern North China Craton. • Craton destruction within 20–40 Myr requires a density exceeding the underlying mantle and viscosity below 10²² Pa s • A flat slab may have hydrated the eastern part of the North China Craton, weakening it and promoting thinning and destruction. • Rapid weakening likely resulted from accelerated hydration, aided by extensive magmatism that enhanced fluid pathways. • Presence of only a high density lower crust or weak mid-lithospheric discontinuity does not cause craton destruction.

Source: Tectonophysics

DOI: 10.1016/j.tecto.2025.230756

Authors: Jyotirmoy Paul, Arne Spang, Andrea Piccolo

Institutions: University of Oslo, University of Bayreuth, University of Leeds

Language: English

Topic: Geological and Geochemical Analysis

Subfield: Geophysics

Field: Earth and Planetary Sciences

Domain: Physical Sciences

Open Access status: hybrid

Estimated APC paid: $3,190

Funders: Royal Society, Deutsche Forschungsgemeinschaft