<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">465791255</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180323112025.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170327e19900201xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/BF00306440</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/BF00306440</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Meta-igneous origin of Hercynian peraluminous granites in N.W. French Massif Central: implications for crustal history reconstructions</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Laurent Turpin, Michel Cuney, Marc Friedrich, Jean-Luc Bouchez, Monique Aubertin]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">Seventy samples of Hercynian peraluminous granites (Guéret, Millevaches and Saint Sylvestre massifs) and metamorphic units of the Limousin area were analysed for Rb−Sr and Sm−Nd. The source rocks of the peraluminous granites can be found in the metamorphic rocks of Limousin, among them meta-igneous rocks were largely predominent over meta-sedimentary rocks in the source of the three granites. Millevaches and Guéret granites were generated by the partial melting of rocks comprising meta-volcanics and meta-sediments, whereas the Saint Sylvestre granite was produced exclusively by the melting of late Precambrian granites. This leads to confusing T DM Nd values, the confusion being amplified by the segregation of monazite during the petrogenetic evolution of the peraluminous granites, which leads to dramatic fractionation in Sm/Nd ratios. The data of the present study tend to demonstrate that peraluminous granites do not give a good representation of isotopic mean crustal estimates. Late Precambrian time seems, however, to have been a period of extensive crustal generation in Western Europe.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Springer-Verlag, 1990</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Turpin</subfield>
   <subfield code="D">Laurent</subfield>
   <subfield code="u">Centre d'Etudes Nucléaires Valrho, DEAEA-SEA, B.P. 171, F-30205, Bagnols-sur-Cèze, France</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Cuney</subfield>
   <subfield code="D">Michel</subfield>
   <subfield code="u">CREGU G.S. CNRS-GREGU, B.P. 23, F-54501, Vandoeuvre Cedex, France</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Friedrich</subfield>
   <subfield code="D">Marc</subfield>
   <subfield code="u">CREGU G.S. CNRS-GREGU, B.P. 23, F-54501, Vandoeuvre Cedex, France</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Bouchez</subfield>
   <subfield code="D">Jean-Luc</subfield>
   <subfield code="u">Laboratoire de Pétrophysique et Tectonique, Université Paul Sabatier, 38, Rue des Trente-Six Ponts, F-34000, Toulouse, France</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Aubertin</subfield>
   <subfield code="D">Monique</subfield>
   <subfield code="u">Section d'Analyses Isotopiques et Nucléaires, CEA/IRDÍ, Bâtiment 391, CEN, Saclay, F-91191, Gif sur Yvette, France</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Contributions to Mineralogy and Petrology</subfield>
   <subfield code="d">Springer-Verlag</subfield>
   <subfield code="g">104/2(1990-02-01), 163-172</subfield>
   <subfield code="x">0010-7999</subfield>
   <subfield code="q">104:2&lt;163</subfield>
   <subfield code="1">1990</subfield>
   <subfield code="2">104</subfield>
   <subfield code="o">410</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/BF00306440</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/BF00306440</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">Turpin</subfield>
   <subfield code="D">Laurent</subfield>
   <subfield code="u">Centre d'Etudes Nucléaires Valrho, DEAEA-SEA, B.P. 171, F-30205, Bagnols-sur-Cèze, France</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">Cuney</subfield>
   <subfield code="D">Michel</subfield>
   <subfield code="u">CREGU G.S. CNRS-GREGU, B.P. 23, F-54501, Vandoeuvre Cedex, France</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">Friedrich</subfield>
   <subfield code="D">Marc</subfield>
   <subfield code="u">CREGU G.S. CNRS-GREGU, B.P. 23, F-54501, Vandoeuvre Cedex, France</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">Bouchez</subfield>
   <subfield code="D">Jean-Luc</subfield>
   <subfield code="u">Laboratoire de Pétrophysique et Tectonique, Université Paul Sabatier, 38, Rue des Trente-Six Ponts, F-34000, Toulouse, France</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">Aubertin</subfield>
   <subfield code="D">Monique</subfield>
   <subfield code="u">Section d'Analyses Isotopiques et Nucléaires, CEA/IRDÍ, Bâtiment 391, CEN, Saclay, F-91191, Gif sur Yvette, France</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">Contributions to Mineralogy and Petrology</subfield>
   <subfield code="d">Springer-Verlag</subfield>
   <subfield code="g">104/2(1990-02-01), 163-172</subfield>
   <subfield code="x">0010-7999</subfield>
   <subfield code="q">104:2&lt;163</subfield>
   <subfield code="1">1990</subfield>
   <subfield code="2">104</subfield>
   <subfield code="o">410</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>
