Experimental deformation of serpentinite and its tectonic implications

TLDR

Serpentinite weakens and embrittles when dehydrated because pore pressure reduces effective confining pressure and structural changes lower cohesive strength. The study experimentally tests serpentinite strength and ductility up to 700 °C and 5 kbar to clarify its role in mountain building. Experiments show serpentinite has granite‑like strength at room temperature but weakens and becomes brittle above 300–600 °C due to dehydration to forsterite and talc, implying that dehydration‑induced embrittlement can localize deformation and enable tectonic emplacement of alpine‑type serpentinites at those temperatures.

Abstract

Experimental investigation into the strength and ductility of serpentinite at temperatures to 700°C and confining pressures to 5 kb has yielded results important to the understanding of the role of serpentinite in orogenesis. Sealed specimens of antigorite-chrysotile serpentinite, with ultimate strength comparable to that of granite at room temperature, showed a marked weakening above 500–600°C; a mesh-textured serpentinite containing lizardite, chrysotile, and a minor amount of brucite showed a similar loss of strength at 300–350°C. Brittleness always accompanied the high-temperature weakening, although the samples showing high strength at lower temperatures were often ductile. Petrographic and X-ray examinations reveal that serpentine in the weakened and embrittled specimens has undergone partial dehydration to forsterite and talc. The embrittlement and weakening is attributed to a reduction in the effective confining pressure due to the pore pressure of the water released during dehydration and to a loss in cohesive strength due to changes in the structure upon dehydration. The hypothesis of tectonic emplacement of serpentinites of the alpine type thus becomes highly plausible at temperatures great enough for dehydration weakening, while being difficult to accept at lower temperatures where the strength of the serpentinite is high. Weakening upon heating to the appropriate dehydration temperature in the range 300–600°C of a partially serpentinized oceanic lower crust or upper mantle should also serve to concentrate deformation in the heated belt, thus facilitating mountain building. The embrittlement associated with dehydration extends the maximum theoretical depth for brittle fracture in the mantle to that of the deepest hydrated phases.