- IGSN: IEDRM00C1
- classification: volcanic:basaltic
- physical-form: hand specimen
- quantity (g): 378.23
- description: Araragiyama lava
- modified at 2020-02-13
Table 1. Whole-rock compositions of Numaura lava, Araragiyama lava, and later L-2 stage lavas < 20190621121300-423166 > in Kuritani et al. (2008)refreshed at 2020-07-30
1: Nm 10 2: Nm 18 3: Nm 19 4: Nm 20 5: Nm 21 6: Nm43 7: Nm44 8: Sn 14 9: Sn 22 10: Sn 25 11: Nm 1 12: Nm 7 13: Nm 8 14: Nm 9 15: Nm 13 16: Nm 17 17: Nm 23 18: Nm 24 19: Sn 1 20: Sn 2 21: Sn 12 22: Sn 15 23: Sn 16 24: On 7 25: On 11 26: Sn 29 27: Sn 32
(a) XRF procedures of Takei (2002) on XRF PANalytical PW2400
(b) Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006) on Q-ICPMS Agilent 7500cs
(c) Q-ICP-MS_procedures of Lu et al. (2007) on Q-ICPMS Agilent 7500cs
(d) U-Series_procedures of Yokoyama et al. (1999, 2001, 2003) on TIMS Finnigan MAT261, MAT262 and Triton TI
(e) Sr isotopes_procedures of Yoshikawa and Nakamura (1993) on TIMS Finnigan MAT261, MAT262 and Triton TI
(f) Nd isotopes_procedures of Nakamura et al. (1991, 2003) on TIMS Finnigan MAT261, MAT262 and Triton TI
(g) Pb isotopes_procedures of Kuritani and Nakamura (2002, 2003) on TIMS Finnigan MAT261, MAT262 and Triton TI
@article{20151111092049-344692,
author={{Sn 2}},
title={Hand specimen with quantity 378.23 g at \nolinkurl{/ISEI/stone storage/Room A/2F/A/2/Kuritani 26/}},
journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20151111092049-344692}{DREAM}},
volume={20},
pages={20151111092049-344692},
year={2015},
url={http://dream.misasa.okayama-u.ac.jp/?q=20151111092049-344692},
}<?xml version="1.0" encoding="UTF-8"?>
<acquisitions>
<acquisition>
<global_id>20190621120931-739145</global_id>
<name>Sn 2</name>
<device>XRF PANalytical PW2400</device>
<technique>XRF procedures of Takei (2002)</technique>
<operator>Kuritani</operator>
<sample_global_id>20151111092049-344692</sample_global_id>
<sample_name>Sn 2</sample_name>
<description/>
<chemistries>
<analysis>
<nickname>SiO2</nickname>
<value>49.17</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>TiO2</nickname>
<value>1.07</value>
<unit>%</unit>
<uncertainty/>
<label/>
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<analysis>
<nickname>Al2O3</nickname>
<value>17.06</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Fe2O3T</nickname>
<value>10.69</value>
<unit>%</unit>
<uncertainty/>
<label/>
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<analysis>
<nickname>MnO</nickname>
<value>0.18</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>MgO</nickname>
<value>8.09</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>CaO</nickname>
<value>9.46</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Na2O</nickname>
<value>3.21</value>
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<uncertainty/>
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<analysis>
<nickname>K2O</nickname>
<value>0.76</value>
<unit>%</unit>
<uncertainty/>
<label/>
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<analysis>
<nickname>P2O5</nickname>
<value>0.25</value>
<unit>%</unit>
<uncertainty/>
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</analysis>
<analysis>
<nickname>LOI</nickname>
<value>0.42</value>
<unit>%</unit>
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<analysis>
<nickname>total</nickname>
<value>100.36</value>
<unit>%</unit>
<uncertainty/>
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<analysis>
<nickname>Cr</nickname>
<value>283.0</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ni</nickname>
<value>142.0</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
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</acquisition>
<acquisition>
<global_id>20190621141352-270134</global_id>
<name>Sn 2</name>
<device>Q-ICPMS Agilent 7500cs</device>
<technique>Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006)</technique>
<operator>Kuritani</operator>
<sample_global_id>20151111092049-344692</sample_global_id>
<sample_name>Sn 2</sample_name>
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<analysis>
<nickname>Li</nickname>
<value>5.88</value>
<unit>ppm</unit>
<uncertainty/>
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<analysis>
<nickname>Be</nickname>
<value>0.9</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Rb</nickname>
<value>18.2</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Sr</nickname>
<value>392.0</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Y</nickname>
<value>27.9</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Cs</nickname>
<value>0.87</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ba</nickname>
<value>174.0</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>La</nickname>
<value>11.6</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ce</nickname>
<value>27.0</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pr</nickname>
<value>3.47</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Nd</nickname>
<value>15.6</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Sm</nickname>
<value>3.65</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Eu</nickname>
<value>1.33</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Gd</nickname>
<value>4.08</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Tb</nickname>
<value>0.7</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Dy</nickname>
<value>4.33</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ho</nickname>
<value>0.95</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Er</nickname>
<value>2.64</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Tm</nickname>
<value>0.41</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Yb</nickname>
<value>2.78</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Lu</nickname>
<value>0.42</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pb</nickname>
<value>1.83</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Th</nickname>
<value>1.67</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>U</nickname>
<value>0.49</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
</chemistries>
</acquisition>
<acquisition>
<global_id>20190621141410-933000</global_id>
<name>Sn 2</name>
<device>Q-ICPMS Agilent 7500cs</device>
<technique>Q-ICP-MS_procedures of Lu et al. (2007)</technique>
<operator>Kuritani</operator>
<sample_global_id>20151111092049-344692</sample_global_id>
<sample_name>Sn 2</sample_name>
<description/>
<chemistries>
<analysis>
<nickname>B</nickname>
<value>5.55</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Zr</nickname>
<value>104.0</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Hf</nickname>
<value>2.31</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>Nb</nickname>
<value>4.09</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ta</nickname>
<value>0.28</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
</chemistries>
</acquisition>
<acquisition>
<global_id>20190621150437-474200</global_id>
<name>Sn 2</name>
<device>TIMS Finnigan MAT261, MAT262 and Triton TI</device>
<technique>Sr isotopes_procedures of Yoshikawa and Nakamura (1993)</technique>
<operator>Kuritani</operator>
<sample_global_id>20151111092049-344692</sample_global_id>
<sample_name>Sn 2</sample_name>
<description/>
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<analysis>
<nickname>Sr87zSr86</nickname>
<value>0.703169</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
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</acquisition>
<acquisition>
<global_id>20190621150604-337373</global_id>
<name>Sn 2</name>
<device>TIMS Finnigan MAT261, MAT262 and Triton TI</device>
<technique>Pb isotopes_procedures of Kuritani and Nakamura (2002, 2003)</technique>
<operator>Kuritani</operator>
<sample_global_id>20151111092049-344692</sample_global_id>
<sample_name>Sn 2</sample_name>
<description/>
<chemistries>
<analysis>
<nickname>Pb206zPb204</nickname>
<value>18.366</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pb207zPb204</nickname>
<value>15.518</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pb208zPb204</nickname>
<value>38.249</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
</chemistries>
</acquisition>
<acquisition>
<global_id>20190621150616-493695</global_id>
<name>Sn 2</name>
<device>TIMS Finnigan MAT261, MAT262 and Triton TI</device>
<technique>Nd isotopes_procedures of Nakamura et al. (1991, 2003)</technique>
<operator>Kuritani</operator>
<sample_global_id>20151111092049-344692</sample_global_id>
<sample_name>Sn 2</sample_name>
<description/>
<chemistries>
<analysis>
<nickname>Nd143zNd144</nickname>
<value>0.512929</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
</chemistries>
</acquisition>
</acquisitions>
place quantity
ISEI/stone storage/Room A/2F/A/2/Kuritani 26 over 1 year
2020-12-25 15:45 2022-07-30 04:26
description:
ISEI/main/--/D/4/Kuritani 26 about 5 years
2015-11-11 09:52 2020-12-25 15:45
description:
ISEI/main/--/Kuritani 26 31 minutes
2015-11-11 09:20 2015-11-11 09:52
description: