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 1S(a). Major element compositions of olivine grains from San Bartolo lava < 20200226101942-797330 >
pub
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<nickname>FeO</nickname>
<value>8.01</value>
<unit>%</unit>
<uncertainty/>
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<nickname>MnO</nickname>
<value>0.14</value>
<unit>%</unit>
<uncertainty/>
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<nickname>CaO</nickname>
<value>0.24</value>
<unit>%</unit>
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<nickname>NiO</nickname>
<value>0.22</value>
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<nickname>modeOfOlFo</nickname>
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<nickname>SiO2</nickname>
<value>40.85</value>
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<nickname>MgO</nickname>
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<nickname>FeO</nickname>
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<nickname>MnO</nickname>
<value>0.22</value>
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<nickname>CaO</nickname>
<value>0.13</value>
<unit>%</unit>
<uncertainty/>
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<nickname>NiO</nickname>
<value>0.32</value>
<unit>%</unit>
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<value>85.7</value>
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<nickname>SiO2</nickname>
<value>40.21</value>
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<nickname>MgO</nickname>
<value>45.27</value>
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<nickname>FeO</nickname>
<value>12.79</value>
<unit>%</unit>
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<nickname>MnO</nickname>
<value>0.29</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<nickname>CaO</nickname>
<value>0.24</value>
<unit>%</unit>
<uncertainty/>
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<analysis>
<nickname>NiO</nickname>
<value>0.12</value>
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<nickname>modeOfOlFo</nickname>
<value>90.6</value>
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<uncertainty/>
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<nickname>SiO2</nickname>
<value>41.06</value>
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<nickname>MgO</nickname>
<value>49.62</value>
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<nickname>FeO</nickname>
<value>7.99</value>
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<nickname>MnO</nickname>
<value>0.15</value>
<unit>%</unit>
<uncertainty/>
<label/>
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<nickname>CaO</nickname>
<value>0.21</value>
<unit>%</unit>
<uncertainty/>
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<nickname>NiO</nickname>
<value>0.25</value>
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<nickname>modeOfOlFo</nickname>
<value>84.4</value>
<unit>%</unit>
<uncertainty/>
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<nickname>SiO2</nickname>
<value>39.96</value>
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<nickname>MgO</nickname>
<value>44.15</value>
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<nickname>FeO</nickname>
<value>14.61</value>
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<nickname>MnO</nickname>
<value>0.27</value>
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<nickname>CaO</nickname>
<value>0.25</value>
<unit>%</unit>
<uncertainty/>
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<nickname>NiO</nickname>
<value>0.16</value>
<unit>%</unit>
<uncertainty/>
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<value>40.4</value>
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<nickname>MgO</nickname>
<value>45.18</value>
<unit>%</unit>
<uncertainty/>
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<nickname>FeO</nickname>
<value>13.52</value>
<unit>%</unit>
<uncertainty/>
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<nickname>MnO</nickname>
<value>0.21</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<nickname>CaO</nickname>
<value>0.18</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>SiO2</nickname>
<value>40.25</value>
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<value>0.26</value>
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<value>0.17</value>
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<value>0.14</value>
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<value>85.5</value>
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<value>12.63</value>
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<value>0.27</value>
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<nickname>CaO</nickname>
<value>0.2</value>
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<nickname>NiO</nickname>
<value>0.18</value>
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<nickname>modeOfOlFo</nickname>
<value>89.3</value>
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<nickname>SiO2</nickname>
<value>40.5</value>
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<nickname>MgO</nickname>
<value>48.92</value>
<unit>%</unit>
<uncertainty/>
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<nickname>FeO</nickname>
<value>8.84</value>
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<nickname>MnO</nickname>
<value>0.11</value>
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<uncertainty/>
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<nickname>CaO</nickname>
<value>0.21</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>NiO</nickname>
<value>0.17</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>modeOfOlFo</nickname>
<value>85.3</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>SiO2</nickname>
<value>40.39</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<nickname>MgO</nickname>
<value>46.14</value>
<unit>%</unit>
<uncertainty/>
<label/>
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<nickname>FeO</nickname>
<value>12.45</value>
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<uncertainty/>
<label/>
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<nickname>MnO</nickname>
<value>0.18</value>
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<uncertainty/>
<label/>
<info/>
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<nickname>CaO</nickname>
<value>0.16</value>
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<uncertainty/>
<label/>
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<analysis>
<nickname>NiO</nickname>
<value>0.13</value>
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<uncertainty/>
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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.