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

H Jung - Geosciences Journal, 2017 - Springer
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 …

The petrologic and petrochronologic record of progressive vs polyphase deformation: Opening the analytical toolbox

S Oriolo, B Schulz, M Hueck, P Oyhantcabal… - Earth-Science …, 2022 - Elsevier
The concepts of progressive and polyphase deformation have been widely applied by
structural geologists to explain complexly deformed rocks, particularly for ductile conditions …

Relationships between olivine CPO and deformation parameters in naturally deformed rocks and implications for mantle seismic anisotropy

RE Bernard, WM Behr, TW Becker… - Geochemistry …, 2019 - Wiley Online Library
We analyze peridotites from a wide range of tectonic settings to investigate relationships
between olivine crystallographic preferred orientation (CPO) and deformation conditions in …

[HTML][HTML] Southern Tibetan rifting since late Miocene enabled by basal shear of the underthrusting Indian lithosphere

B Zhang, X Bao, Y Wu, Y Xu, W Yang - Nature Communications, 2023 - nature.com
Syncontractional extension is prominent in present-day Tibet, but its origin remains
vigorously debated. Several deep-seated geodynamic processes (eg, Indian underthrusting …

Modeling olivine CPO evolution with complex deformation histories: Implications for the interpretation of seismic anisotropy in the mantle

Y Boneh, LFG Morales, E Kaminski… - Geochemistry …, 2015 - Wiley Online Library
Relating seismic anisotropy to mantle flow requires detailed understanding of the
development and evolution of olivine crystallographic preferred orientation (CPO). Recent …

Inferring upper-mantle flow from seismic anisotropy: an experimental perspective

P Skemer, LN Hansen - Tectonophysics, 2016 - Elsevier
Patterns of mantle flow are most directly inferred from observations of seismic anisotropy,
which is mainly caused by the crystallographic preferred orientation (CPO) of olivine, the …

A review of mechanisms generating seismic anisotropy in the upper mantle

LN Hansen, M Faccenda, JM Warren - Physics of the Earth and Planetary …, 2021 - Elsevier
Seismic anisotropy is a key observational tool for mapping flow in Earth's upper mantle.
However, interpreting patterns of anisotropy relies on a firm understanding of the …

The seismic structure of the Antarctic upper mantle

DA Wiens, W Shen, AJ Lloyd - 2023 - pubs.geoscienceworld.org
The deployment of seismic stations and the development of ambient noise tomography as
well as new analysis methods provide an opportunity for higher-resolution imaging of …

Axial‐type olivine crystallographic preferred orientations: The effect of strain geometry on mantle texture

V Chatzaras, SC Kruckenberg… - Journal of …, 2016 - Wiley Online Library
The effect of finite strain geometry on crystallographic preferred orientation (CPO) is poorly
constrained in the upper mantle. Specifically, the relationship between shape preferred …

Upper mantle anisotropic shear velocity structure at the equatorial Mid‐Atlantic Ridge constrained by Rayleigh wave group velocity analysis from the PI‐LAB …

U Saikia, C Rychert, N Harmon… - Geochemistry …, 2021 - Wiley Online Library
The evolution of ocean lithosphere and asthenosphere are fundamental to plate tectonics,
yet high resolution imaging is rare. We present shear wave velocity and azimuthal …