The history of ocean basins
@inproceedings{Hess1962TheHO, title={The history of ocean basins}, author={Harry Hammond Hess}, year={1962} }
A mechanical load sensing arrangement is disposed at the buoy tow point and is coupled to the tow cable. This load sensing arrangement is mechanically displaced proportional to tensile loading of the cable. A mechanical stabilizer fin attitude control arrangement is interconnected between the stabilizer fin and the load sensing arrangement. The attitude control arrangement is responsive to the mechanical displacement of the load sensing arrangement to control the stabilizer fin to assume a low…
727 Citations
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References
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ABSTRACT The present sediment thicknesses in deep-sea basins, away from continents and islands, are apt to be the total thicknesses of the first two (or more) layers revealed by seismic surveys. The…
A new dynamic conception of the internal constitution of the earth
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SummaryA new conception of dynamic character is given for the internal constitution of the Earth. The main feature of the conception is that the material composition of the Earth becomes more and…
Calculations on the thermal history of the Earth
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The possible thermal history of a spherically symmetric earth is studied by comparing numerical calculations of the development of temperature within a number of model earths with observations on the…
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On the Mid-Pacific and Capricorn expeditions seismic-refraction observations were made at 42 stations scattered widely within an area of the Central Equatorial Pacific Ocean extending from latitudes…
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- 1954
temperature correspond well to the position of Gould's Belt at these longitudes and lend additional support to the hypothesis of a "local system" or give evidence for some definite feature of local…
SEISMIC-REFRACTION MEASUREMENTS IN THE ATLANTIC OCEAN BASINS, IN THE MEDITERRANEAN SEA, ON THE MID-ATLANTIC RIDGE, AND IN THE NORWEGIAN SEA
- Geology
- 1959
Seismic-refraction measurements in the western basins of the North Atlantic Ocean show that an average crustal section consists of ½–l km of low-velocity sediments and 4–6 km of oceanic crustal rock…
Some geochemical aspects of the Mohorovicic discontinuity
- Geology
- 1960
Hypotheses of mantle composition and of the nature of the Mohorovicic discontinuity are discussed.
It is considered (a) that there is no evidence for the assumption that meteorite compositions can…
The AMSOC hole to the Earth's mantle
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- 1959
It was July 1957 in Washington, D. C., when the Earth Sciences panel of the National Science Foundation (NSF) had just completed two days of hard work evaluating some 60 odd projects requesting…