Major element concentrations in spinel, olivine and pyroxene from peridotites of ODP Hole 210-1277 of the Newfoundland margin ...

Serpentinized spinel peridotites of the Newfoundland margin drilled during ODP Leg 210 at Site 1277 have preserved, relic mineral compositions similar to the most depleted abyssal peridotites worldwide and different from those of the conjugate Iberian margin. The samples are derived from mass flows...

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Main Authors: Müntener, Othmar, Manatschal, Gianreto
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2006
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.707815
https://doi.pangaea.de/10.1594/PANGAEA.707815
id ftdatacite:10.1594/pangaea.707815
record_format openpolar
spelling ftdatacite:10.1594/pangaea.707815 2023-05-15T17:17:47+02:00 Major element concentrations in spinel, olivine and pyroxene from peridotites of ODP Hole 210-1277 of the Newfoundland margin ... Müntener, Othmar Manatschal, Gianreto 2006 application/zip https://dx.doi.org/10.1594/pangaea.707815 https://doi.pangaea.de/10.1594/PANGAEA.707815 en eng PANGAEA https://dx.doi.org/10.1016/j.epsl.2006.10.009 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg210 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 2006 ftdatacite https://doi.org/10.1594/pangaea.70781510.1016/j.epsl.2006.10.009 2023-04-03T13:12:12Z Serpentinized spinel peridotites of the Newfoundland margin drilled during ODP Leg 210 at Site 1277 have preserved, relic mineral compositions similar to the most depleted abyssal peridotites worldwide and different from those of the conjugate Iberian margin. The samples are derived from mass flows containing clasts of peridotite and gabbro and from in-situ basement, and are mostly mylonitic cpx-poor spinel harzburgites with Cr-rich spinels (Cr#0.35-0.66). Melting of the Newfoundland mantle occurred in the spinel peridotite field and probably exceeded the cpx-out phase boundary for some samples. Using proposed spinel peridotite melting models and experimentally derived phase diagrams, the Newfoundland harzburgites can be modeled as a residue after extraction of 14 to 20-25% melting. Basalts that are interleaved with mass flow deposits on top of the peridotite basement resemble normal to transitional mid-ocean ridge basalt. This, together with the unusually high Cr# of some spinel harzburgites suggest that ... : Supplement to: Müntener, Othmar; Manatschal, Gianreto (2006): High degrees of melt extraction recorded by spinel harzburgite of the Newfoundland margin: The role of inheritance and consequences for the evolution of the southern North Atlantic. Earth and Planetary Science Letters, 252(3-4), 437-452 ... Article in Journal/Newspaper Newfoundland North Atlantic DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg210
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg210
Joides Resolution
Ocean Drilling Program ODP
Müntener, Othmar
Manatschal, Gianreto
Major element concentrations in spinel, olivine and pyroxene from peridotites of ODP Hole 210-1277 of the Newfoundland margin ...
topic_facet Drilling/drill rig
Leg210
Joides Resolution
Ocean Drilling Program ODP
description Serpentinized spinel peridotites of the Newfoundland margin drilled during ODP Leg 210 at Site 1277 have preserved, relic mineral compositions similar to the most depleted abyssal peridotites worldwide and different from those of the conjugate Iberian margin. The samples are derived from mass flows containing clasts of peridotite and gabbro and from in-situ basement, and are mostly mylonitic cpx-poor spinel harzburgites with Cr-rich spinels (Cr#0.35-0.66). Melting of the Newfoundland mantle occurred in the spinel peridotite field and probably exceeded the cpx-out phase boundary for some samples. Using proposed spinel peridotite melting models and experimentally derived phase diagrams, the Newfoundland harzburgites can be modeled as a residue after extraction of 14 to 20-25% melting. Basalts that are interleaved with mass flow deposits on top of the peridotite basement resemble normal to transitional mid-ocean ridge basalt. This, together with the unusually high Cr# of some spinel harzburgites suggest that ... : Supplement to: Müntener, Othmar; Manatschal, Gianreto (2006): High degrees of melt extraction recorded by spinel harzburgite of the Newfoundland margin: The role of inheritance and consequences for the evolution of the southern North Atlantic. Earth and Planetary Science Letters, 252(3-4), 437-452 ...
format Article in Journal/Newspaper
author Müntener, Othmar
Manatschal, Gianreto
author_facet Müntener, Othmar
Manatschal, Gianreto
author_sort Müntener, Othmar
title Major element concentrations in spinel, olivine and pyroxene from peridotites of ODP Hole 210-1277 of the Newfoundland margin ...
title_short Major element concentrations in spinel, olivine and pyroxene from peridotites of ODP Hole 210-1277 of the Newfoundland margin ...
title_full Major element concentrations in spinel, olivine and pyroxene from peridotites of ODP Hole 210-1277 of the Newfoundland margin ...
title_fullStr Major element concentrations in spinel, olivine and pyroxene from peridotites of ODP Hole 210-1277 of the Newfoundland margin ...
title_full_unstemmed Major element concentrations in spinel, olivine and pyroxene from peridotites of ODP Hole 210-1277 of the Newfoundland margin ...
title_sort major element concentrations in spinel, olivine and pyroxene from peridotites of odp hole 210-1277 of the newfoundland margin ...
publisher PANGAEA
publishDate 2006
url https://dx.doi.org/10.1594/pangaea.707815
https://doi.pangaea.de/10.1594/PANGAEA.707815
genre Newfoundland
North Atlantic
genre_facet Newfoundland
North Atlantic
op_relation https://dx.doi.org/10.1016/j.epsl.2006.10.009
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.70781510.1016/j.epsl.2006.10.009
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