Erratum to: Crystal preferred orientations of olivine, orthopyroxene, serpentine, chlorite, and amphibole, and implications for seismic anisotropy in subduction zones: a review

Abstract

There are errors in the article entitled "Crystal preferred orientations of olivine, orthopyroxene, serpentine, chlorite, and amphibole, and implications for seismic anisotropy in subduction zones: a review" by Haemyeong Jung, which appeared on pages 985-1011 of the December issue in 2017. The author has provided a corrected article which is attached at the end of this erratum. ABSTRACT:This study provides a comprehensive review of the crystal preferred orientation (CPO) of olivine and orthopyroxene in the upper mantle, and of several hydrous minerals in the mantle wedge and at the slab-mantle interface. It discusses the seismic anisotropy of those minerals. Water-induced CPOs of olivine produced by previous experimental studies under high pressure and temperature conditions were found in many natural rocks. It is emphasized that the strong CPOs of hydrous minerals such as serpentine, chlorite, and amphibole, play an important role in interpreting the anomalously strong seismic anisotropy observed in subduction zones.

Thermal Conductivity of Hydrous Wadsleyite Determined by Non‐Equilibrium Molecular Dynamics Based on Machine Learning

“…Zhang, Schmandt, & Zhang, 2021) and direct interaction between slabs and the surrounding mantle could cause the development of the lattice-preferred orientation (LPO), which may lead to anisotropic thermal conductivity within and around the slab. Olivine has a dominant slip system of (010)[100] under dry conditions (Type-A, [010] axis is subnormal to the shear plane and [100] axis is subparallel to the shear direction) (Jung, 2018), and a dominant slip system of (010)[001] under high stress with different water contents (Type-B) (Jung & Karato, 2001). Type-AG is also called Type A + B, with [010] axis being strongly subnormal to the plane, and can be formed when the water content changes (Jung, 2018).…”

“…The thermal conductivity of ringwoodite is isotropic, and it has a higher thermal conductivity under low temperatures, which allows the colder slab to heat up faster than the benchmark. The actual LPO may be only ∼20% of the single crystal alignment as inferred from the P-wave anisotropy (Jung, 2018;Jung et al, 2006;W.-Y. Zhou et al, 2021).…”

“…Olivine has a dominant slip system of (010)[100] under dry conditions (Type-A, [010] axis is subnormal to the shear plane and [100] axis is subparallel to the shear direction) (Jung, 2018), and a dominant slip system of (010)[001] under high stress with different water contents (Type-B) (Jung & Karato, 2001). Type-AG is also called Type A + B, with [010] axis being strongly subnormal to the plane, and can be formed when the water content changes (Jung, 2018). reported that Type-C olivine fabric ((100)[001] slip system) was developed under high pressure (11.1-12.7 GPa), but olivine in the cold slab has transformed into wadsleyite with a positive Clapeyron slope at this pressure (Katsura & Ito, 1989).…”

Petrology and Tectonic Geophysics of Massive and Foliated Eclogites in the North Qilian Orogenic Belt: Changes in Mineral Composition, Oxygen Fugacity, and Fabric during Exhumation

“…Many prob-lems are difficult to solve by traditional methods. Since in situ Lu-Hf isotope analysis of zircon is often used in current analysis, the following mainly introduces the in situ Lu-Hf isotope analysis of zircon [29][30][31][32][33].…”