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Geology; April 1998; v. 26; no. 4; p. 311-314
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Long-term and short-term global Cenozoic sea-level estimates

Michelle A. Kominz, Kenneth G. Miller, and James V. Browning

Rutgers University, Department of Geological Sciences, Piscataway, NJ, United States

Backstripping analysis of three continuously cored, well-dated boreholes from the New Jersey Coastal Plain (Ocean Drilling Program [ODP] Leg 150X) indicates a long-term (10 8 -10 7 yr) eustatic fall of nearly equal 100 m since 55 Ma (early Eocene) and suggests short-term (0.5-3 m.y.) eustatic falls of less than nearly equal 70 m. Eustatic estimates are calculated from residuals between the decompacted, unloaded, and paleodepth-corrected records and tectonic subsidence (assuming a cooling lithospheric plate). Because the residuals are similar among the three sites, we interpret them as an approximation of the eustatic signal.

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