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The relative timing of serpentinisation and mantle exhumation at the ocean-continent transition, Iberia: constraints from oxygen isotopes
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
2000 (English)In: EARTH AND PLANETARY SCIENCE LETTERS, ISSN 0012-821X, Vol. 178, no 3-4, 327-338 p.Article in journal (Refereed) Published
Abstract [en]

Legs 173 and 149 of the Ocean Drilling Program profiled a zone of exhumed mantle peridotite at the ocean-continent transition (OCT) beneath the Iberia Abyssal Plain. The zone of exhumed peridotite appears to be tens of kilometers wide and is situated betw

Place, publisher, year, edition, pages
ELSEVIER SCIENCE BV , 2000. Vol. 178, no 3-4, 327-338 p.
Keyword [en]
oceanic crust; continental crust; serpentinite; exhumation; oxygen; isotopes; fluid dynamics; HYDROTHERMAL ALTERATION; CRUSTAL STRUCTURE; DETACHMENT FAULT; CORE COMPLEXES; STABLE ISOTOPE; MARGINS; SERPENTINIZATION; FRACTIONATION; METAMORPHISM; GENERATION
Identifiers
URN: urn:nbn:se:uu:diva-37756OAI: oai:DiVA.org:uu-37756DiVA: diva2:65655
Note
Addresses: Skelton ADL, Uppsala Univ, Dept Earth Sci, Villavagen 16, S-75236 Uppsala, Sweden. Uppsala Univ, Dept Earth Sci, S-75236 Uppsala, Sweden. Univ Wisconsin, Dept Geol & Geophys, Madison, WI 53706 USA.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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