georefid:2003-063772SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=2003-0637722001-01-01publicationgeorefid:2003-063772Hebert, RejeanUniversite Laval, Departement de Geologie et de Genie geologique, Ste-Foy, QC, CanadaauthorGueddari, K.Southampton Oceanography Center, United KingdomauthorLafleche, M. R.University of Hawaii, United StatesauthorBeslier, M. O.University of Bonn, Federal Republic of GermanyauthorGardien, V.Centre Geoscientifique de Quebec, CanadaauthorGeological Society of London, London, United KingdompublisherdocumentHardcopyIn: Wilson, R. C. L. (editor), Whitmarsh, R. B. (editor), Taylor, B. (editor), Froitzheim, N. (editor), Non-volcanic rifting of continental margins; a comparison of evidence from land and sea187161-189Ultramafic and mafic rocks recovered at Holes 1068A and 1070A were drilled during Leg 173 of the Ocean Drilling Program (ODP) in the ocean-continent transition zone of the Iberia Abyssal Plain. Peridotites show contrasting petrographic characteristics. Hole 1068A peridotites are fine grained and show a well-defined high-temperature foliation marked by elongated pyroxene as well as aligned spinels. Hole 1068A peridotites are strongly serpentinized. Hole 1070A peridotites are coarse grained and show little evidence of high-temperature foliation. The degree of serpentinization is lower and relicts of silicate minerals are preserved. In both sets of recovered material, spinels show a wide range of composition and suggest a complex magmatic evolution. Gabbros dykes, which are found only in Hole 1070A, are very coarse grained and are locally sheared and/or crushed. Magmatic amphiboles are kaersutites and Ti-rich tschermakites that are partially replaced by hornblende and actinolite, and are associated with plagioclase of intermediate composition. Peridotites and pyroxenite have low TiO (sub 2) , Al (sub 2) O (sub 3) and CaO contents in carbonate-free samples. Ni and Cr contents fall into the upper-mantle array. On the other hand, gabbros have relatively high TiO (sub 2) and V contents reflecting modal ilmenite, and suggesting that they are relatively differentiated. This paper presents the very first geochemical data on platinum group elements (PGE) of peridotites and gabbros from passive margins. Peridotites and gabbros show low PGE (25.83 ppb and 1.44 ppb), Pd (2.75 ppb and 0.15 ppb), Pd/Ir ratios (1.45 and 1.3) and mafic index. Pyroxenite has the highest PGE (27.97 ppb), Pd/Ir (19.87) and Pt/Ir (10.25). Interelemental correlation and observation of PGE-bearing sulphide phases suggest that the PGE are hosted by single sulphide phases. From a PGE point of view, extraction of magmas involved very PGE-depleted liquids similar to gabbroic veins cutting the peridotites at Hole 1070A. Partial melting is interpreted as occurring just before oceanic accretion. Geochemical attributes suggest that the peridotites belong to the Ronda and Beni Bousera peridotitic depleted end-member clan. Thus they are believed to be of subcontinental origin. Deformation and retrograde metamorphism of peridotites and gabbros are consistent with exhumation in a rift environment post-dating the 120 Ma magmatic stage.completedIgneous and metamorphic petrologySolid-earth geophysicsAtlantic Oceanchemical compositioncontinental crustcontinental margincrustEast AtlanticEuropegabbrosIberian abyssal plainIberian Peninsulaigneous rocksLeg 173mantlemineral compositionNorth AtlanticNortheast AtlanticOcean Drilling Programoceanic crustODP Site 1068ODP Site 1070passive marginsperidotitespetrographyplate tectonicsplutonic rocksPortugalSouthern EuropeSpainultramaficsupper mantleurn:org.iodp:exp:173urnlargerWorkCitationcampaignurn:org.iodp:exp:173:site:1068urnlargerWorkCitationstudyurn:org.iodp:exp:173urnlargerWorkCitationcampaignurn:org.iodp:exp:173:site:1070urnlargerWorkCitationstudyurn:org.iodp:exp:173urnlargerWorkCitationcampaignEnglishgeoscientificInformation-12.4326-11.364340.405740.4747