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  • 173-1068; 173-1070; COMPCORE; Composite Core; Joides Resolution; Leg173; Ocean Drilling Program; ODP; South Atlantic Ocean  (1)
  • 21.60.CS  (1)
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 334 (1989), S. 365-376 
    ISSN: 1434-601X
    Keywords: 20.40. + z ; 23.20.-g ; 21.60.CS
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract A spectroscopic study is performed for high spin states of55Fe,55Co and57Ni. To populate the investigated residues with a relevant cross section, the fusion evaporation reactions of30Si(28Si, 2pn)55Fe,30Si(28Si, 2np)55Co and4He(54Fe,n)57Ni were chosen. To identify the newγ transitions and to build the energy level schemes,γ — γ coincidence techniques together with excitation functions were employed. Angular distributions andγ — γ angular correlations allowed us to assign the spin values of the nuclear states. The previous level scheme of55Fe is extended into the region between 6.5–11 MeV of excitation energy, up to spin 27/2, while the yrast decay paths of57Ni and55Co are reported here for the first time. Experimental data are fairly well reproduced by Glaudemans' shell model calculations.
    Type of Medium: Electronic Resource
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  • 2
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    PANGAEA
    In:  Supplement to: Skelton, Alsadair SL; Valley, John W (2000): The relative timing of serpentinisation and mantle exhumation at the ocean-continent transition, Iberia: constraints from oxygen isotopes. Earth and Planetary Science Letters, 178(3-4), 327-338, https://doi.org/10.1016/S0012-821X(00)00087-X
    Publication Date: 2024-01-09
    Description: 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 between blocks of continental crust and the first products of ocean accretion. Exhumed peridotite is 95-100% serpentinised to probable depths of 2-3 km. Down core oxygen isotope profiles of serpentinised peridotite at Sites 1068 and 1070 (Leg 173) show evidence for two fluid infiltration events. The earlier event involved pervasive infiltration of comparatively warm (〉175°C) sea water and accompanied serpentinisation. The later event involved structurally focused infiltration of comparatively cool (650-150°C) sea water and accompanied active mantle exhumation. We therefore conclude that the uppermost mantle was serpentinised before it was exhumed at the Iberian OCT. Implicit to this conclusion is that a sizeable region of serpentinised mantle existed directly beneath thinned but intact continental crust. Serpentinite has comparatively low density, low frictional strength and low permeability. The presence of such a "soft" layer may have localised deformation and consequently promoted detachment-style exhumation of the uppermost mantle. The low permeability of a serpentinite 'cap' layer might help to explain the lack of observed melt at the Iberian OCT.
    Keywords: 173-1068; 173-1070; COMPCORE; Composite Core; Joides Resolution; Leg173; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 4 datasets
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