<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">465723950</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180323111724.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170327e19900701xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/BF02295927</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/BF02295927</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Temperature paleogradient estimations in the central Bohemian basin</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[J. Šafanda, B. Žáková, G. Buntebarth]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">Summary: The coalification data of 12 boreholes in the Central Bohemian Basin are used to evaluate the paleotemperature gradients for the Upper Carboniferous period of the basin's development. Two versions of the burial history considered are supposed to yield an upper and a lower estimate. According to the more probable &quot;lower” version, the average values of the paleogradient suggest an increasing tendency from west to east in the interval of 45-53K/km. The current geothermal gradients vary in the range of 28-35K/km. By combining the present thermal conductivity and the paleogradients, we have tried to estimate the Upper Carboniferous heat flow. Its values range from 96mW/m 2 to 117mW/m 2 . The results obtained can be compared with the paleogradient estimates in the Saar-Nahe Basin (F. R. of Germany). This region, which is similar with respect to the time of origin and tectonic pattern to the Central Bohemian Basin, displays on the average a slightly higher Permo-Carboniferous geothermal gradient of 60K/km.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Academia, Publishing House of the Czechoslovak Academy of Sciences, 1990</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Šafanda</subfield>
   <subfield code="D">J.</subfield>
   <subfield code="u">Geophysical Inst., Czechosl. Acad. Sci., Prague, Boční II/1401, 141 31, Praha 4, Czechoslovakia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Žáková</subfield>
   <subfield code="D">B.</subfield>
   <subfield code="u">Geoindustria Praha s. p., Argentinská 34, 170 04, Praha 7, Czechoslovakia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Buntebarth</subfield>
   <subfield code="D">G.</subfield>
   <subfield code="u">Institut für Geophysik, Arnold-Sommerfeld Str. 1, D-3392, Clausthal-Zellerfeld, F. R. of Germany</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Studia Geophysica et Geodaetica</subfield>
   <subfield code="d">Kluwer Academic Publishers</subfield>
   <subfield code="g">34/3(1990-07-01), 208-219</subfield>
   <subfield code="x">0039-3169</subfield>
   <subfield code="q">34:3&lt;208</subfield>
   <subfield code="1">1990</subfield>
   <subfield code="2">34</subfield>
   <subfield code="o">11200</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/BF02295927</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/BF02295927</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">Šafanda</subfield>
   <subfield code="D">J.</subfield>
   <subfield code="u">Geophysical Inst., Czechosl. Acad. Sci., Prague, Boční II/1401, 141 31, Praha 4, Czechoslovakia</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">Žáková</subfield>
   <subfield code="D">B.</subfield>
   <subfield code="u">Geoindustria Praha s. p., Argentinská 34, 170 04, Praha 7, Czechoslovakia</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">Buntebarth</subfield>
   <subfield code="D">G.</subfield>
   <subfield code="u">Institut für Geophysik, Arnold-Sommerfeld Str. 1, D-3392, Clausthal-Zellerfeld, F. R. of Germany</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">Studia Geophysica et Geodaetica</subfield>
   <subfield code="d">Kluwer Academic Publishers</subfield>
   <subfield code="g">34/3(1990-07-01), 208-219</subfield>
   <subfield code="x">0039-3169</subfield>
   <subfield code="q">34:3&lt;208</subfield>
   <subfield code="1">1990</subfield>
   <subfield code="2">34</subfield>
   <subfield code="o">11200</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>
