Formation of lithospheric detachments: quantifying the mechanical effect of hydration reactions
Abstract
Many authors have published experimentally determined flow laws of rheologically important monophase aggregates
and polyphase rocks. These laws provide good first order constraints on lithology-controlled lithospheric
strength variations. However, since the whole range of mineralogical and chemical rock compositions cannot
be experimentally tested, variations in reaction-controlled rock strength cannot be systematically and fully
characterized.
We here present the results of a study coupling thermodynamical and Thermomechanical modelling aiming
at predicting the mechanical impact of metamorphic reactions on the strength of the mantle during its exhumation
in rifted zones.
Thermodynamic modelling is used for calculating the mineralogical composition of a typical peridotite as
a function of pressure, temperature and water content. For a given P-T condition, the calculated modes and
flow laws parameters for each phase constituting the paragenesis are then used as input of the Minimized
Power Geometric model for predicting the polyphase aggregate strength. Hence, by considering P-T evolutions
characteristic of exhumed mantle, we quantify the strength of the mantle as a function of pressure, temperature
and hydration history in a rift zone. The mechanical impact of such metamorphic reactions and hydration is first
quantified in 1D for three simplified hydration schemes and then introduced in preliminary 2D models which
coupled fluid transfer to the thermodynamically derived rheological parameters. Schemes with limited hydratation
are found to keep rocks in condition close to brittle ductile transition for a longer time and to permit more efficient
mantle exhumation