Elastic Anisotropy of Lizardite at Subduction Zone Conditions

Deng, Xin; Luo, Chenxing; Wentzcovitch, Renata M.; Abers, Geoffrey A.; Wu, Zhongqing

doi:10.1029/2022gl099712

Elastic Anisotropy of Lizardite at Subduction Zone Conditions

Journal Article · Mon Aug 29 00:00:00 EDT 2022 · Geophysical Research Letters

DOI:https://doi.org/10.1029/2022gl099712· OSTI ID:1978577

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Univ. of Science and Technology of China, Hefei (China); OSTI
Columbia Univ., New York, NY (United States)
Columbia Univ., New York, NY (United States); Columbia Univ., Palisades, NY (United States), Lamont–Doherty Earth Observatory
Cornell Univ., Ithaca, NY (United States)
Univ. of Science and Technology of China, Hefei (China)

Subduction zones transport water into Earth's deep interior through slab subduction. Serpentine minerals, the primary hydration product of ultramafic peridotite, are abundant in most subduction zones. Characterization of their high-temperature elasticity, particularly their anisotropy, will help us better estimate the extent of mantle serpentinization and the Earth's deep water cycle. Lizardite, the low-temperature polymorph of serpentine, is stable under the P-T conditions of cold subduction slabs (<260°C at 2 GPa), and its high-temperature elasticity remains unknown. Here we report ab initio elasticity and acoustic wave velocities of lizardite at P-T conditions of subduction zones. Our static results agree with previous studies. Its high-temperature velocities are much higher than previous experimental-based lizardite estimates with chrysotile but closer to antigorite velocities. The elastic anisotropy of lizardite is much larger than that of antigorite and could better account for the observed large shear-wave splitting in some cold slabs such as Tonga.

View Accepted Manuscript (DOE)

Research Organization:: Columbia Univ., New York, NY (United States)

Sponsoring Organization:: USDOE Office of Science (SC)

Grant/Contract Number:: SC0019759

OSTI ID:: 1978577

Alternate ID(s):: OSTI ID: 1887313

Journal Information:: Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 18 Vol. 49; ISSN 0094-8276

Publisher:: American Geophysical Union (AGU)Copyright Statement

Country of Publication:: United States

Language:: English

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Elastic Anisotropy of Lizardite at Subduction Zone Conditions

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