The Othris Ophiolite, Greece: A snapshot of subduction initiation at a mid-ocean ridge

M.G. Barth; P.R.D. Mason; G.R. Davies; M.R. Drury

doi:10.1016/j.lithos.2007.06.018

The Othris Ophiolite, Greece: A snapshot of subduction initiation at a mid-ocean ridge

M.G. Barth, P.R.D. Mason, G.R. Davies, M.R. Drury

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

The mantle section of the Tethyan-type Othris Ophiolite, Greece, records tectono-magmatic processes characteristic of both mid-ocean ridges and supra-subduction zones. The Othris Ophiolite is a remnant of the Jurassic Neotethys Ocean, which existed between Eurasia and Gondwanaland. Othris peridotites range from fertile plagioclase lherzolites to depleted harzburgites. Abundances of Al

Original language	English
Pages (from-to)	234-254
Journal	Lithos
Volume	100
DOIs	https://doi.org/10.1016/j.lithos.2007.06.018
Publication status	Published - 2008

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title = "The Othris Ophiolite, Greece: A snapshot of subduction initiation at a mid-ocean ridge",

abstract = "The mantle section of the Tethyan-type Othris Ophiolite, Greece, records tectono-magmatic processes characteristic of both mid-ocean ridges and supra-subduction zones. The Othris Ophiolite is a remnant of the Jurassic Neotethys Ocean, which existed between Eurasia and Gondwanaland. Othris peridotites range from fertile plagioclase lherzolites to depleted harzburgites. Abundances of Al",

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AU - Davies, G.R.

AU - Drury, M.R.

PY - 2008

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AB - The mantle section of the Tethyan-type Othris Ophiolite, Greece, records tectono-magmatic processes characteristic of both mid-ocean ridges and supra-subduction zones. The Othris Ophiolite is a remnant of the Jurassic Neotethys Ocean, which existed between Eurasia and Gondwanaland. Othris peridotites range from fertile plagioclase lherzolites to depleted harzburgites. Abundances of Al

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DO - 10.1016/j.lithos.2007.06.018

M3 - Article

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SP - 234

EP - 254

JO - Lithos

JF - Lithos

ER -

The Othris Ophiolite, Greece: A snapshot of subduction initiation at a mid-ocean ridge

Abstract

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