Abstract
Site 664 is located at 0°06.44'N, 23°13.65'W, in a water depth of 3806.3 m in the central equatorial Atlantic on the upper-middle flank of the E side of the mid-Atlantic Ridge just N of the Romanche Fracture Zone. Although basement outcroppings are common in the surrounding terrain, the region immediately adjacent to Site 664 is largely covered with sediments. Our primary objective at this site was to obtain late Neogene records of the equatorial divergence and of eolian sedimentation. -from Authors
Cite
CITATION STYLE
Ruddiman, W., Sarnthein, M., & Baldauf, J. (1988). Site 664. Proc., Initial Reports (Part A), ODP, Leg 108, Eastern Tropical Atlantic. (Section 2), 619–740. https://doi.org/10.2973/odp.proc.ir.108.109.1988
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