Controls on the rheological properties of peridotite at a palaeosubduction interface: A transect across the base of the Oman–UAE ophiolite

Controls on the rheological properties of peridotite at a palaeosubduction interface: A transect across the base of the Oman–UAE ophiolite

<p>Studies of experimentally deformed rocks and small-scale natural shear zones have demonstrated that volumetrically minor phases can control strain localisation by limiting grain growth and promoting grain-size sensitive deformation mechanisms. These small-scale studies are often used to inf...

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Những tác giả chính:	Ambrose, T, Wallis, D, Hansen, L, Waters, D, Searle, M
Định dạng:	Journal article
Được phát hành:	Elsevier 2018

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