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These rocks are represented by veins or patches which can be reported to be related to oxide gabbros in Hole 735B (Dick et al., 2000) and with olivine gabbro in Hole 1105A (Casey et al., 2007) but are found associated with or reducing each rock types in Gap U1473A. The diploma to which the igneous layering right here and in Holes 735B and 1105A will be interpreted when it comes to magmatic sedimentation as seen in layered intrusions is problematic and sometimes

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