5. Site 11541

Shipboard Scientific Party2

PRINCIPAL RESULTS

Site 1154 is located in Zone A, somewhat east of the locus of the residual depth anomaly. It lies ~70 km east of Site 1153, on seafloor of approximately the same age (~28 Ma). Seafloor in this region is characterized by a northeast-trending series of deep en echelon, east-west oriented grabens. The oblique trend and en echelon arrangement of the grabens suggest that they formed as failed rift grabens associated with a westward propagating rift. To the east, seafloor fabric appears normal, typical of Zone A. This is the third site in the initial east-west transect designed to locate the Indian/Pacific mantle boundary across the northern part of our operational area.

Between 0 and ~233 meters below seafloor (mbsf), we recovered a single wash core containing reddish brown pelagic clay overlying calcareous ooze, but the boundaries and the thicknesses of these units are unknown. From ~233 to ~266 mbsf, 9.4 m of light gray, moderately plagioclase-olivine phyric pillow basalt, with occasional glassy rims and slight to moderate alteration, was recovered. The hole was abandoned at ~266 mbsf as the >6000-m drill string was approaching its safe working limits.

Two handpicked glasses and three whole-rock powders were analyzed on board. The glasses are slightly more evolved than those from Site 1153, with 7.6-7.8 wt% MgO. The whole rocks have significantly less MgO (~6.0 wt%) and higher K2O than the glasses but are otherwise similar in composition. As at Site 1153, these compositional differences are likely the result of alteration of the whole-rock groundmass.

Overall, Site 1154 glass compositions are offset from those of Site 1153 along low-pressure crystal fractionation trends; these trends are offset to generally higher incompatible element contents from those of the 0- to 7-Ma Zone A lavas. These observations suggest that, at ~28 Ma, Zone A lavas were derived from uniform parental magma compositions, as they are today, but their source mantle was somewhat more fertile. On the Ba vs. Zr/Ba diagram, Site 1154 glasses are distinctly Pacific in character.

1Examples of how to reference the whole or part of this volume can be found under "Citations" in the preliminary pages of the volume.
2Shipboard Scientific Party addresses can be found under "Shipboard Scientific Party" in the preliminary pages of the volume.

Ms 187IR-105

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