Last edited by Nimuro
Monday, April 20, 2020 | History

4 edition of Surface-ship gravity measurements in the North Atlantic Ocean 1965 and 1968 found in the catalog.

Surface-ship gravity measurements in the North Atlantic Ocean 1965 and 1968

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  • 27 Currently reading

Published by Bianco Lunos Bogtrykkeri in København .
Written in English

    Places:
  • North Atlantic Ocean.
    • Subjects:
    • Gravity -- North Atlantic Ocean.

    • Edition Notes

      Includes bibliographical references.

      Statementby Ole Bedsted Andersen.
      SeriesGeodætisk instituts skrifter ;, 3 række, bd. 41
      Classifications
      LC ClassificationsQB1 .D25 bd. 41, QB337.5.A8 .D25 bd. 41
      The Physical Object
      Pagination47 p., [3] fold. leaves :
      Number of Pages47
      ID Numbers
      Open LibraryOL4933157M
      ISBN 108774500287
      LC Control Number76360023

      Nabighian Etal Gravity | Pendulum | Accelerometer Geofisica5/5(1). Sitting almost in the middle of the Atlantic Ocean, between Africa and Brazil, is a speck of rock named Ascension Island. It was mid-September and the frigid spray from the North Sea deposited a dew like film on the sailor's dark pea coat. In an hour the giant "SS," identifying the sub as American, had been painted over on both Author: Oldmaninthedesert.


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Surface-ship gravity measurements in the North Atlantic Ocean 1965 and 1968 by Ole Bedsted Andersen Download PDF EPUB FB2

Andersen, O.B.:Surface Ship Gravity Measurements in the North Atlantic Ocean and Geodaetisk Institut Skrifter, Raekke 3, Bind XLI. Google ScholarCited by: 5. Full text of "Sea surface topography from space" See other formats.

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The submarine pendulum gravity measurements of Vening Meinesz are mainly of historical interest today. The first gravimeters installed in surface ships appeared during the 's. These early ocean surface gravity measurements were only of modest accuracy and, again, now are mainly of historical value.

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arctic domain A hydrographic division sometimes used in the North Atlantic Ocean to distinguish it from the polar domain to the north and the Atlantic domain to the south.

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