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Hole 479 in the Guaymas Basin of the Gulf of California (27°50.8'N, 111°37.5'W) was drilled using the conventional DSDP rotary coring process, recovering 62% of the section. Although coring disturbance in the top 26 cores precluded paleomagnetic analysis, the remainder of the section (250-440 m sub-bottom) contained indurated, relatively undisturbed sediment with abundant, well-preserved laminae suitable for sampling. Since the age of the section and sedimentation rates were not well constrained, we examined the magnetostratigraphy of the lower part of the section to locate the Brunhes/Matuyama boundary or other magnetic markers.

Paleomagnetism of Laminated Sediments from the Guaymas Basin, Gulf of California, Deep Sea Drilling Project Site 479