Volume 40 Issue 10
Oct 2026
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MA Junsheng, LIU Chuanjiang, WANG Duojun, CAI Nao, ZHANG Rui. Elastic Wave Velocities of Lawsonite and Its Implications for Seismic Velocity Anomalies in Subduction Zones[J]. Chinese Journal of High Pressure Physics, 2026, 40(10): 101201. doi: 10.11858/gywlxb.20261006
Citation: MA Junsheng, LIU Chuanjiang, WANG Duojun, CAI Nao, ZHANG Rui. Elastic Wave Velocities of Lawsonite and Its Implications for Seismic Velocity Anomalies in Subduction Zones[J]. Chinese Journal of High Pressure Physics, 2026, 40(10): 101201. doi: 10.11858/gywlxb.20261006

Elastic Wave Velocities of Lawsonite and Its Implications for Seismic Velocity Anomalies in Subduction Zones

doi: 10.11858/gywlxb.20261006
  • Received Date: 08 Jan 2026
  • Rev Recd Date: 08 Feb 2026
  • Accepted Date: 16 Sep 2026
  • Available Online: 09 Mar 2026
  • Issue Publish Date: 22 Oct 2026
  • Lawsonite is a key hydrous mineral in subducting oceanic crust, with an H2O mass fraction of up to 11.5% and volume fractions that can reach 50%, and is stable over a wide pressure-temperature range. Constraining the high-pressure elastic properties of lawsonite is therefore essential for understanding seismic velocity structures in subduction zones and the deep-water cycle. In this study, dense polycrystalline lawsonite was synthesized by hot-pressing natural lawsonite powder at 7 GPa and 1 073 K for 2 h. Ultrasonic interferometry was then used to measure P- and S-wave velocities of lawsonite up to 8 GPa at room temperature, from which the elastic moduli and their pressure derivatives were determined. The results show that both elastic wave velocities and moduli increase with pressure, the adiabatic bulk modulus and shear modulus are 120(1) and 51(1) GPa at room temperature and ambient pressure, and their derivatives with respect to pressure are 5.7(1) and 0.9(1), respectively. Using these elastic properties, together with previous mineral-physics results, we constructed a lawsonite-bearing eclogite model, which indicates that the presence of lawsonite can provide a plausible explanation for the seismic velocity anomalies observed at depths of about 60–90 km within intermediate-temperature subducting slabs such as Nicaragua.

     

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