I strongly believe that post cruise data-processing is less complete and less
precise when compared to that which is done immediately on board while our
minds and our energy are focused on the mission at hand. This is especially true
for the interpretation of images from the sea floor and for mapping done by
manned and unmanned engines, such as submersibles and robots.
References
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Limited, New York, p 354
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15:195–213
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Heezen BC, Hollister CD (1971) The face of the deep. Oxford University Press, Oxford, 159, P
Opdyke ND, Hekinian R (1967) Magnetic properties of some igneous rocks from the MidAtlantic Ridge. J Geophys Res 78(8):2257–2260
Vine FJ, Matthews DH (1963) Magnetic anomalies over oceanic ridges. Nature 199:947
Wilson JT (1963) A possible origin of the Hawaiian Islands. Can J Phys 41:863–870
Wilson JT (1965) A new class of faults and their bearing on continental drift. Nature 207:343–347
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Communicating Scientific Results
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