. Collected reprints, Essa Institute for Oceanography. Oceanography MAGNETIC ANOMALIES IN THE GULF OF MEXICO 521 east-west strike at about 25°N and an offset of 200 to 300 km [Murray, 1961]. No evidence of a seaward extension of this feature can be claimed from the marine magnetic data. Al- though there is a change in the direction of widely spaced contours, as drawn, at this lati- tude, the positional uncertainty in these con- tours precludes any conclusion about their sig- nificance. The extremely featureless magnetic field in the. Fig. 2. Magnetic total intensity anomalies of
. Collected reprints, Essa Institute for Oceanography. Oceanography MAGNETIC ANOMALIES IN THE GULF OF MEXICO 521 east-west strike at about 25°N and an offset of 200 to 300 km [Murray, 1961]. No evidence of a seaward extension of this feature can be claimed from the marine magnetic data. Al- though there is a change in the direction of widely spaced contours, as drawn, at this lati- tude, the positional uncertainty in these con- tours precludes any conclusion about their sig- nificance. The extremely featureless magnetic field in the. Fig. 2. Magnetic total intensity anomalies of the northwest Gulf. Solid lines segments are ships' tracks. Broken line segments are aeromagnetic tracks. Solid curved lines are magnetic contours (values in gammas) and broken curved lines are less reliable magnetic Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Institute for Oceanography; Atlantic Oceanographic Laboratories (U. S. ); Pacific Oceanographic Laboratories; United States. Environmental Science Services Administration. Research Laboratories. Washington, D. C. : U. S. Dept. of Commerce, Environmental Science Services Administration, Research Laboratories : For sale by the Supt. of Docs. , U. S. G. P. O.
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