Schiavi et al. (2011) Trace element and Pb–B–Li isotope systematics of olivine-hosted melt inclusions: insights into source metasomatism beneath Stromboli (southern Italy), Contributions to Mineralogy and Petrology, 163, doi:10.1007/s00410-011-0713-5. < 20200225102214-755085 > pub
Table 2S(a). Major element compositions of olivine grains from pumice samples < 20200226102333-675017 >
pub
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<nickname>FeO</nickname>
<value>10.19</value>
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<nickname>MnO</nickname>
<value>0.27</value>
<unit>%</unit>
<uncertainty/>
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<nickname>CaO</nickname>
<value>0.29</value>
<unit>%</unit>
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<nickname>NiO</nickname>
<value>0.09</value>
<unit>%</unit>
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<nickname>modeOfOlFo</nickname>
<value>84.4</value>
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<nickname>SiO2</nickname>
<value>39.38</value>
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<nickname>MgO</nickname>
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<nickname>FeO</nickname>
<value>14.72</value>
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<nickname>MnO</nickname>
<value>0.31</value>
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<nickname>CaO</nickname>
<value>0.3</value>
<unit>%</unit>
<uncertainty/>
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<nickname>NiO</nickname>
<value>0.19</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<nickname>modeOfOlFo</nickname>
<value>85.9</value>
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<nickname>SiO2</nickname>
<value>39.44</value>
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<nickname>MgO</nickname>
<value>44.92</value>
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<nickname>FeO</nickname>
<value>13.17</value>
<unit>%</unit>
<uncertainty/>
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<analysis>
<nickname>MnO</nickname>
<value>0.27</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>CaO</nickname>
<value>0.29</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>NiO</nickname>
<value>0.09</value>
<unit>%</unit>
<uncertainty/>
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<nickname>modeOfOlFo</nickname>
<value>83.7</value>
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<uncertainty/>
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<nickname>SiO2</nickname>
<value>40.77</value>
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<nickname>MgO</nickname>
<value>44.83</value>
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<nickname>FeO</nickname>
<value>15.51</value>
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<uncertainty/>
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<nickname>MnO</nickname>
<value>0.25</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>CaO</nickname>
<value>0.29</value>
<unit>%</unit>
<uncertainty/>
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<nickname>NiO</nickname>
<value>0.15</value>
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<uncertainty/>
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<sample_global_id>20200226094045-091484</sample_global_id>
<sample_name>ol52a</sample_name>
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<analysis>
<nickname>modeOfOlFo</nickname>
<value>84.6</value>
<unit>%</unit>
<uncertainty/>
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<info/>
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<nickname>SiO2</nickname>
<value>39.85</value>
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<uncertainty/>
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<nickname>MgO</nickname>
<value>44.79</value>
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<nickname>FeO</nickname>
<value>14.51</value>
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<nickname>MnO</nickname>
<value>0.28</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>CaO</nickname>
<value>0.27</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<nickname>NiO</nickname>
<value>0.11</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<nickname>modeOfOlFo</nickname>
<value>84.6</value>
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<nickname>SiO2</nickname>
<value>39.85</value>
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<uncertainty/>
<label/>
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<nickname>MgO</nickname>
<value>44.79</value>
<unit>%</unit>
<uncertainty/>
<label/>
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<analysis>
<nickname>FeO</nickname>
<value>14.51</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<nickname>MnO</nickname>
<value>0.28</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>CaO</nickname>
<value>0.27</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>NiO</nickname>
<value>0.19</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<nickname>modeOfOlFo</nickname>
<value>84.6</value>
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<nickname>SiO2</nickname>
<value>39.85</value>
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<value>44.79</value>
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<value>0.27</value>
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<nickname>modeOfOlFo</nickname>
<value>83.4</value>
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<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>SiO2</nickname>
<value>39.2</value>
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<uncertainty/>
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<analysis>
<nickname>MgO</nickname>
<value>43.5</value>
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<nickname>FeO</nickname>
<value>15.38</value>
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<nickname>MnO</nickname>
<value>0.16</value>
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<nickname>CaO</nickname>
<value>0.29</value>
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<analysis>
<nickname>modeOfOlFo</nickname>
<value>89.4</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>SiO2</nickname>
<value>40.35</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>MgO</nickname>
<value>48.88</value>
<unit>%</unit>
<uncertainty/>
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<nickname>FeO</nickname>
<value>10.32</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>MnO</nickname>
<value>0.13</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<nickname>CaO</nickname>
<value>0.28</value>
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<uncertainty/>
<label/>
<info/>
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<sample_global_id>20200226094045-611687</sample_global_id>
<sample_name>ol127</sample_name>
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<analysis>
<nickname>modeOfOlFo</nickname>
<value>84.9</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>SiO2</nickname>
<value>39.56</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>MgO</nickname>
<value>44.88</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>FeO</nickname>
<value>14.22</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>MnO</nickname>
<value>0.18</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>CaO</nickname>
<value>0.26</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
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<sample_global_id>20200226094045-515116</sample_global_id>
<sample_name>ol129</sample_name>
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<chemistries>
<analysis>
<nickname>modeOfOlFo</nickname>
<value>82.5</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>SiO2</nickname>
<value>39.19</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>MgO</nickname>
<value>43.52</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>FeO</nickname>
<value>16.41</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>MnO</nickname>
<value>0.14</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>CaO</nickname>
<value>0.23</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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The table is created from analysis shown below. The rowname major-Ol (Schiavi et al., 2012) filters out analysis. Upper analysis has priority.To list more analysis, add a stone in stone sub-tab.