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 …

Imaging upper mantle anisotropy with traveltime and splitting intensity observations from teleseismic shear waves: insights from tomographic reconstructions of …

BP VanderBeek, RL Bue, F Rappisi… - Geophysical Journal …, 2023 - academic.oup.com
Teleseismic traveltime tomography remains one of the most popular methods for obtaining
images of Earth's upper mantle. However, despite extensive evidence for an elastically …

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 …

[HTML][HTML] On constraining 3D seismic anisotropy in subduction, mid-ocean-ridge, and plume environments with teleseismic body wave data

M Faccenda, BP VanderBeek - Journal of Geodynamics, 2023 - Elsevier
Conventional seismic tomography studies consider the Earth's interior as mechanically
isotropic, despite seismic anisotropy being widely observed. This current standard approach …

Numerical simulation of 3-D mantle flow evolution in subduction zone environments in relation to seismic anisotropy beneath the eastern Mediterranean region

JM Confal, M Faccenda, T Eken, T Taymaz - Earth and Planetary Science …, 2018 - Elsevier
Seismic anisotropy is a key parameter in understanding subduction zone dynamics in
relation to the recent deformation history. It is usually controlled by the mantle flow patterns …

Crustal anisotropy and deformation of the southeastern Tibetan Plateau revealed by seismic anisotropy of mylonitic amphibolites

B Huang, B Zhang, J Zhang, S Liu, L Zhang… - Journal of Structural …, 2022 - Elsevier
The composition and deformation patterns in the deep crust of southeastern Tibet are
remain controversial. In this study, we present microstructures, fabric and seismic properties …

The Cascadia Paradox: Mantle flow and slab fragmentation in the Cascadia subduction system

MD Long - Journal of Geodynamics, 2016 - Elsevier
The pattern of mantle flow in subduction systems and the processes that control the mantle
flow field represent fundamental but still poorly understood aspects of subduction dynamics …

The peridotite deformation cycle in cratons and the deep impact of subduction

EJ Chin, B Chilson-Parks, Y Boneh, G Hirth, AE Saal… - Tectonophysics, 2021 - Elsevier
Xenoliths play a crucial role in interpretation of mantle deformation and geochemistry. The
classic work of Mercier and Nicolas (1975) introduced the concept of the peridotite …