<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">469025719</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180323132729.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170328e19920701xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/BF02482664</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/BF02482664</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Marine terraces as indicators of global geoidal and hydrological changes</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Yu. Tarakanov, R. Klige, A. Selivanov]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">Spatial pattern analysis of marine terrace elevations from 40-30 thous. years BP was used to reconstruct sea level/geoid surface and geoid parameters during that time. The polar flattening of geodetic ellipsoid was lower than its present value (1/298.81 and 1/298.26) respectively because of glacial-induced mass redistribution. Increase in polar stress occurred during the last 30 thous. years was possibly driven by pertubation brought to the gravitational field by disintegration of polar ice sheets in the Northern hemisphere. But the polar flattening value becomes only half-restored during the last deglacial hemicycle. So repetitive glacial advances during Pleistocene acted as a global &quot;pump” for uncondensed zones at the upper/lower mantle boundary. Dissipation of tidal energy is an order of magnitude less intensive in its Earth's rotation effect.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Kluwer Academic Publishers, 1992</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Tarakanov</subfield>
   <subfield code="D">Yu</subfield>
   <subfield code="u">Academy of Sciences, Earth Physics Institute, 10 Bolshaya Gruzinskaya, Moscow, Russia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Klige</subfield>
   <subfield code="D">R.</subfield>
   <subfield code="u">Moscow University, 119899, Moscow, Russia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Selivanov</subfield>
   <subfield code="D">A.</subfield>
   <subfield code="u">Academy of Sciences, Water Problems Institute, 13/3 Sadovo-Chernogryazskaya, 103064, Moscow, Russia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">GeoJournal</subfield>
   <subfield code="d">Kluwer Academic Publishers</subfield>
   <subfield code="g">27/3(1992-07-01), 243-246</subfield>
   <subfield code="x">0343-2521</subfield>
   <subfield code="q">27:3&lt;243</subfield>
   <subfield code="1">1992</subfield>
   <subfield code="2">27</subfield>
   <subfield code="o">10708</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/BF02482664</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">856</subfield>
   <subfield code="E">40</subfield>
   <subfield code="u">https://doi.org/10.1007/BF02482664</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Tarakanov</subfield>
   <subfield code="D">Yu</subfield>
   <subfield code="u">Academy of Sciences, Earth Physics Institute, 10 Bolshaya Gruzinskaya, Moscow, Russia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Klige</subfield>
   <subfield code="D">R.</subfield>
   <subfield code="u">Moscow University, 119899, Moscow, Russia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Selivanov</subfield>
   <subfield code="D">A.</subfield>
   <subfield code="u">Academy of Sciences, Water Problems Institute, 13/3 Sadovo-Chernogryazskaya, 103064, Moscow, Russia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">773</subfield>
   <subfield code="E">0-</subfield>
   <subfield code="t">GeoJournal</subfield>
   <subfield code="d">Kluwer Academic Publishers</subfield>
   <subfield code="g">27/3(1992-07-01), 243-246</subfield>
   <subfield code="x">0343-2521</subfield>
   <subfield code="q">27:3&lt;243</subfield>
   <subfield code="1">1992</subfield>
   <subfield code="2">27</subfield>
   <subfield code="o">10708</subfield>
  </datafield>
  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="898" ind1=" " ind2=" ">
   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <subfield code="c">XK010000</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-springer</subfield>
  </datafield>
 </record>
</collection>
