<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">467889902</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180406152746.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170328e20061001xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/s00710-006-0134-8</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/s00710-006-0134-8</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Quartz from Allchar as monitor for cosmogenic 26Al: Geochemical and petrogenetic constraints</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[M. K. Pavićević, V. Cvetković, G. Amthauer, A. Bieniok, B. Boev, F. Brandstätter, M. Götzinger, R. Jelenković, D. Prelević, T. Prohaska]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">Summary: Results of a multidisciplinary study on quartz concentrates (mineralogically separated) and etched concentrates (stoichiometric quartz) from three locations at Allchar (Macedonia) are presented. The investigation of quality and composition of these quartz samples is of great interest because the same material has been previously used as monitor for 26Al Acceleration Mass-Spectrometry (AMS) erosion rate estimates. Two genetically different types of quartz are distinguished in the studied samples which petrologically can be described as hydrothermally altered dacites or quartz latites; i.e. volcanic (QV) and hydrothermal (QH) quartz with relative proportions of QH:QV around 3:2. QH is genetically related to the Allchar Sb-As-Tl-S mineralization having very high Sb (85-785 ppm), As (7.6-78 ppm) and (Tl 3.3-4.0 ppm) contents. This type of quartz is also characterized by very high Li (129-138 ppm), Al (2424-2520 ppm) and Ti (153-219 ppm) concentrations. QV appears to be much less enriched in trace elements having Al and K contents ranging from 0 to 280 ppm and from 50 to 85 ppm, respectively. 26Al AMS measurements were done on the samples containing two genetically different types of quartz but this had no effects on the interpretation and erosion rate determinations. However, the extremely high Al concentrations in the analyzed quartz have generally negative effects, mainly by decreasing 26Al/27Al ratios and thus causing an increase of the detection limit. The disagreement between the results of 26Al AMS analyses and quantitative geomorphologic data for one location is probably caused by different geographical position with respect to the direction of cosmic rays.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Springer-Verlag, 2006</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Pavićević</subfield>
   <subfield code="D">M. K.</subfield>
   <subfield code="u">Division of Mineralogy and Material Sciences, University of Salzburg, Salzburg, Austria</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Cvetković</subfield>
   <subfield code="D">V.</subfield>
   <subfield code="u">Division of Mineralogy and Material Sciences, University of Salzburg, Salzburg, Austria</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Amthauer</subfield>
   <subfield code="D">G.</subfield>
   <subfield code="u">Division of Mineralogy and Material Sciences, University of Salzburg, Salzburg, Austria</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Bieniok</subfield>
   <subfield code="D">A.</subfield>
   <subfield code="u">Division of Mineralogy and Material Sciences, University of Salzburg, Salzburg, Austria</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Boev</subfield>
   <subfield code="D">B.</subfield>
   <subfield code="u">Faculty of Mining and Geology, University of Skopje, Štip, Macedonia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Brandstätter</subfield>
   <subfield code="D">F.</subfield>
   <subfield code="u">Department for Mineralogy and Petrology, Natural History Museum, Vienna, Austria</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Götzinger</subfield>
   <subfield code="D">M.</subfield>
   <subfield code="u">Institute for Mineralogy and Christallography, University of Vienna, Vienna, Austria</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Jelenković</subfield>
   <subfield code="D">R.</subfield>
   <subfield code="u">Faculty of Mining and Geology, University of Belgrade, Belgrade, Serbia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Prelević</subfield>
   <subfield code="D">D.</subfield>
   <subfield code="u">Faculty of Mining and Geology, University of Belgrade, Belgrade, Serbia</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Prohaska</subfield>
   <subfield code="D">T.</subfield>
   <subfield code="u">Division of Analytical Chemistry, Department of Chemistry, VIRIS laboratory, University of Natural Resources and Applied Life Sciences (BOKU), Vienna, Austria</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Mineralogy and Petrology</subfield>
   <subfield code="d">Springer-Verlag</subfield>
   <subfield code="g">88/3-4(2006-10-01), 527-550</subfield>
   <subfield code="x">0930-0708</subfield>
   <subfield code="q">88:3-4&lt;527</subfield>
   <subfield code="1">2006</subfield>
   <subfield code="2">88</subfield>
   <subfield code="o">710</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/s00710-006-0134-8</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/s00710-006-0134-8</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">Pavićević</subfield>
   <subfield code="D">M. K.</subfield>
   <subfield code="u">Division of Mineralogy and Material Sciences, University of Salzburg, Salzburg, Austria</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">Cvetković</subfield>
   <subfield code="D">V.</subfield>
   <subfield code="u">Division of Mineralogy and Material Sciences, University of Salzburg, Salzburg, Austria</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">Amthauer</subfield>
   <subfield code="D">G.</subfield>
   <subfield code="u">Division of Mineralogy and Material Sciences, University of Salzburg, Salzburg, Austria</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">Bieniok</subfield>
   <subfield code="D">A.</subfield>
   <subfield code="u">Division of Mineralogy and Material Sciences, University of Salzburg, Salzburg, Austria</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">Boev</subfield>
   <subfield code="D">B.</subfield>
   <subfield code="u">Faculty of Mining and Geology, University of Skopje, Štip, Macedonia</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">Brandstätter</subfield>
   <subfield code="D">F.</subfield>
   <subfield code="u">Department for Mineralogy and Petrology, Natural History Museum, Vienna, Austria</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">Götzinger</subfield>
   <subfield code="D">M.</subfield>
   <subfield code="u">Institute for Mineralogy and Christallography, University of Vienna, Vienna, Austria</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">Jelenković</subfield>
   <subfield code="D">R.</subfield>
   <subfield code="u">Faculty of Mining and Geology, University of Belgrade, Belgrade, Serbia</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">Prelević</subfield>
   <subfield code="D">D.</subfield>
   <subfield code="u">Faculty of Mining and Geology, University of Belgrade, Belgrade, Serbia</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">Prohaska</subfield>
   <subfield code="D">T.</subfield>
   <subfield code="u">Division of Analytical Chemistry, Department of Chemistry, VIRIS laboratory, University of Natural Resources and Applied Life Sciences (BOKU), Vienna, Austria</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">Mineralogy and Petrology</subfield>
   <subfield code="d">Springer-Verlag</subfield>
   <subfield code="g">88/3-4(2006-10-01), 527-550</subfield>
   <subfield code="x">0930-0708</subfield>
   <subfield code="q">88:3-4&lt;527</subfield>
   <subfield code="1">2006</subfield>
   <subfield code="2">88</subfield>
   <subfield code="o">710</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>
