Lee J, Mookherjee M, Kim T, Jung H, Klemd R (2021)
Publication Type: Journal article
Publication year: 2021
Book Volume: 9
Article Number: 644958
DOI: 10.3389/feart.2021.644958
Subduction zones are often characterized by the presence of strong trench-parallel seismic anisotropy and large delay times. Hydrous minerals, owing to their large elastic anisotropy and strong lattice preferred orientations (LPOs), are often invoked to explain these observations. However, the elasticity and the LPO of chloritoid, which is one of such hydrous phases relevant in subduction zone settings, are poorly understood. In this study, we measured the LPO of polycrystalline chloritoid in natural rock samples, obtained the LPO-induced seismic anisotropy, and evaluated the thermodynamic stability field of chloritoid in subduction zones. The LPO of chloritoid aggregates displayed a strong alignment of the [001] axes subnormal to the rock foliation, with a girdle distribution of the [100] axes and the (010) poles subparallel to the foliation. New elasticity data of single-crystal chloritoid showed a strong elastic anisotropy of chloritoid with 47% for S-waves (V
APA:
Lee, J., Mookherjee, M., Kim, T., Jung, H., & Klemd, R. (2021). Seismic Anisotropy in Subduction Zones: Evaluating the Role of Chloritoid. Frontiers in Earth Science, 9. https://doi.org/10.3389/feart.2021.644958
MLA:
Lee, Jungjin, et al. "Seismic Anisotropy in Subduction Zones: Evaluating the Role of Chloritoid." Frontiers in Earth Science 9 (2021).
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