Evans, Cynthia A; Girardeau, Jacques (1988): Chemistry of peridotites of ODP Hole 103-637A [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.743546, Supplement to: Evans, CA; Girardeau, J (1988): Galicia margin peridotites: undepleted abyssal periodotites from the North Atlantic. In: Boillot, G; Winterer, EL; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 103, 195-207, https://doi.org/10.2973/odp.proc.sr.103.138.1988
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Abstract:
A ridge of peridotite was drilled off of the Galicia margin (Hole 637A) during ODP Leg 103. The ridge is located at the approximate boundary between oceanic and continental crust. This setting is of interest because the peridotite may be representative of upwelling upper mantle beneath an incipient ocean basin. The composition of the Galicia margin peridotite is compared with those of other North Atlantic peridotites.
Hole 637A ultramafic lithologies include clinopyroxene-rich spinel harzburgite and lherzolite, as well as plagioclase-bearing peridotites. Variations in mineral modal abundances and mineral compositions are observed but are not systematic. The peridotites are broadly similar in composition to other peridotites recovered from ocean basins, but the mineral compositions and abundances suggest that they are less depleted in basaltic components than other North Atlantic peridotites by about 10%. In particular, the peridotites are enriched in the magmaphilic elements Na, Al, and Ti, as compared with other abyssal peridotites. The high abundances of these elements suggest that the Hole 637A peridotites had experienced, at most, very small amounts of partial melting prior to their emplacement.
The presence of plagioclase rimming spinel in some samples suggests that the peridotite last equilibrated at about 9 kbar, near the transition between plagioclase- and spinel-peridotite stability fields. Temperatures of equilibration of the peridotite are calculated as 900°-1100°C.
The relatively undepleted composition of the peridotite indicates that it was emplaced at a shallow mantle level under a relatively cool thermal regime and cooled below solidus temperatures without having participated in any significant partial melting and basalt production. This is consistent with the emplacement of the peridotite during incipient rifting of the ocean basin, before a true spreading center was established.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 42.088300 * Longitude: -12.863300
Date/Time Start: 1985-04-28T18:00:00 * Date/Time End: 1985-05-04T21:00:00
Event(s):
103-637A * Latitude: 42.088300 * Longitude: -12.863300 * Date/Time Start: 1985-04-28T18:00:00 * Date/Time End: 1985-05-04T21:00:00 * Elevation: -5321.0 m * Penetration: 285.6 m * Recovery: 116.31 m * Location: South Atlantic Ocean * Campaign: Leg103 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 30 cores; 285.6 m cored; 0 m drilled; 40.7 % recovery
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
5 datasets
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Datasets listed in this publication series
- Evans, CA; Girardeau, J (1988): (Table 3) Representative analyses of clinopyroxene from ODP Site 103-637A peridotites. https://doi.org/10.1594/PANGAEA.743541
- Evans, CA; Girardeau, J (1988): (Table 1) Representative analyses of olivine from ODP Hole 103-637A peridotites. https://doi.org/10.1594/PANGAEA.743539
- Evans, CA; Girardeau, J (1988): (Table 2) Representative analyses of orthopyroxene from ODP Hole 103-637A peridotites. https://doi.org/10.1594/PANGAEA.743540
- Evans, CA; Girardeau, J (1988): (Table 5) Representative analyses of plagioclase from ODP Hole 103-637A peridotites. https://doi.org/10.1594/PANGAEA.743545
- Evans, CA; Girardeau, J (1988): (Table 4) Representative analyses of spinel from ODP Hole 103-637A peridotites. https://doi.org/10.1594/PANGAEA.743544