- IGSN: IEDRM00Y5
- place: N35°20′39.8″, E133°25′41.9″ more
- physical-form: hand specimen
- status: unknown
- age (Ma): >1
- description: Daisen volcanic field; Basalt flows (1.21 Ma)
- modified at 2019-12-13
- surface:
Table 1: Major and trace element concentrations and isotopic ratios in selected Daisen Lavas Feineman, M et al. (2013)
1: 03052804 2: 03052805 3: 03053002 4: 03053003 5: 03060102 6: 03060103A 7: 03060604 8: 02051801 9: 03052002 10: 03052004 11: 03052802 12: 03052803 13: SAN1 14: SAN2 15: 02060707 16: 02060710 17: 02060711 18: 02060713 19: 02080501 20: 03042004 21: 03042005 22: 03042006 23: 03042007 24: 3052810 25: 03052812 26: 02072901
(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) Sr isotopes_procedures of Yoshikawa and Nakamura (1993) on TIMS Finnigan MAT261, MAT262 and Triton TI
(e) Nd isotopes_procedures of Nakamura et al. (1991, 2003) on TIMS Finnigan MAT261, MAT262 and Triton TI
(f) TIMS with double spike correction on TIMS Thermo-Fisher MAT261
(g) U-Series_procedures of Yokoyama et al. (1999, 2001, 2003) on MAT 262
@article{20120820090355-672-993,
author={{03052812}},
title={Hand specimen at \nolinkurl{/ISEI/main/PML-stone-room-111/shelf 8/shelf 8-3/A working box for noble-gas analysis/}},
journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20120820090355-672-993}{DREAM}},
volume={19},
pages={20120820090355-672-993},
year={2012},
url={http://dream.misasa.okayama-u.ac.jp/?q=20120820090355-672-993},
}<?xml version="1.0" encoding="UTF-8"?>
<acquisitions>
<acquisition>
<global_id>20191114110918-053762</global_id>
<name>3052812</name>
<device>TIMS Finnigan MAT261, MAT262 and Triton TI</device>
<technique>Sr isotopes_procedures of Yoshikawa and Nakamura (1993)</technique>
<operator>Maureen Feineman</operator>
<sample_global_id>20120820090355-672-993</sample_global_id>
<sample_name>03052812</sample_name>
<description></description>
<place>
<global_id>20131112140438-435302</global_id>
<name>Daisen volcanic field</name>
<longitude>133.428305555556</longitude>
<latitude>35.3443888888889</latitude>
<elevation>0.0</elevation>
<description> Basalt flows (1.21 Ma)</description>
</place>
<chemistries>
<analysis>
<nickname>Sr87zSr86</nickname>
<value>0.705099</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
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<acquisition>
<global_id>20191114110339-428441</global_id>
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<device>Q-ICPMS Agilent 7500cs</device>
<technique>Q-ICP-MS_procedures of Lu et al. (2007)</technique>
<operator>Maureen Feineman</operator>
<sample_global_id>20120820090355-672-993</sample_global_id>
<sample_name>03052812</sample_name>
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<global_id>20131112140438-435302</global_id>
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<description> Basalt flows (1.21 Ma)</description>
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<chemistries>
<analysis>
<nickname>Zr</nickname>
<value>104.0</value>
<unit>ppm</unit>
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<analysis>
<nickname>Hf</nickname>
<value>2.81</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Nb</nickname>
<value>10.9</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ta</nickname>
<value>0.701</value>
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<acquisition>
<global_id>20191113115402-841786</global_id>
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<description> Basalt flows (1.21 Ma)</description>
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<chemistries>
<analysis>
<nickname>Li</nickname>
<value>6.35</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
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<analysis>
<nickname>Rb</nickname>
<value>29.3</value>
<unit>ppm</unit>
<uncertainty/>
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<analysis>
<nickname>Sr</nickname>
<value>736.0</value>
<unit>ppm</unit>
<uncertainty/>
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<analysis>
<nickname>Y</nickname>
<value>27.4</value>
<unit>ppm</unit>
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<analysis>
<nickname>Cs</nickname>
<value>0.222</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ba</nickname>
<value>467.0</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>La</nickname>
<value>28.2</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ce</nickname>
<value>49.1</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pr</nickname>
<value>7.17</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Nd</nickname>
<value>29.1</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Sm</nickname>
<value>5.77</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>Eu</nickname>
<value>1.94</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Gd</nickname>
<value>5.42</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Tb</nickname>
<value>0.838</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Dy</nickname>
<value>4.88</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ho</nickname>
<value>0.982</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Er</nickname>
<value>2.49</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Tm</nickname>
<value>0.365</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Yb</nickname>
<value>2.41</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Lu</nickname>
<value>0.343</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pb</nickname>
<value>4.9</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Th</nickname>
<value>3.27</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>U</nickname>
<value>0.66</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
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<acquisition>
<global_id>20191114105831-069309</global_id>
<name>3052812</name>
<device>XRF PANalytical PW2400</device>
<technique>XRF procedures of Takei (2002)</technique>
<operator>Maureen Feineman</operator>
<sample_global_id>20120820090355-672-993</sample_global_id>
<sample_name>03052812</sample_name>
<description/>
<place>
<global_id>20131112140438-435302</global_id>
<name>Daisen volcanic field</name>
<longitude>133.428305555556</longitude>
<latitude>35.3443888888889</latitude>
<elevation>0.0</elevation>
<description> Basalt flows (1.21 Ma)</description>
</place>
<chemistries>
<analysis>
<nickname>SiO2</nickname>
<value>49.39</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>TiO2</nickname>
<value>1.35</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>Al2O3</nickname>
<value>17.11</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Fe2O3</nickname>
<value>9.72</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>MnO</nickname>
<value>0.17</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>MgO</nickname>
<value>7.64</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>CaO</nickname>
<value>8.62</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Na2O</nickname>
<value>3.28</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>K2O</nickname>
<value>1.11</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>P2O5</nickname>
<value>0.31</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Cr</nickname>
<value>0.05</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ni</nickname>
<value>0.03</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>LOI</nickname>
<value>1.23</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>total</nickname>
<value>100.01</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
</chemistries>
</acquisition>
<acquisition>
<global_id>20191114111420-665207</global_id>
<name>3052812</name>
<device>TIMS Finnigan MAT261, MAT262 and Triton TI</device>
<technique>Nd isotopes_procedures of Nakamura et al. (1991, 2003)</technique>
<operator>Maureen Feineman</operator>
<sample_global_id>20120820090355-672-993</sample_global_id>
<sample_name>03052812</sample_name>
<description></description>
<place>
<global_id>20131112140438-435302</global_id>
<name>Daisen volcanic field</name>
<longitude>133.428305555556</longitude>
<latitude>35.3443888888889</latitude>
<elevation>0.0</elevation>
<description> Basalt flows (1.21 Ma)</description>
</place>
<chemistries>
<analysis>
<nickname>Nd143zNd144</nickname>
<value>0.512662</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>eNd</nickname>
<value>0.5</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
</chemistries>
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<acquisition>
<global_id>20191114111854-524179</global_id>
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<device>TIMS Thermo-Fisher MAT261</device>
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<operator></operator>
<sample_global_id>20120820090355-672-993</sample_global_id>
<sample_name>03052812</sample_name>
<description></description>
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<global_id>20131112140438-435302</global_id>
<name>Daisen volcanic field</name>
<longitude>133.428305555556</longitude>
<latitude>35.3443888888889</latitude>
<elevation>0.0</elevation>
<description> Basalt flows (1.21 Ma)</description>
</place>
<chemistries>
<analysis>
<nickname>Pb206zPb204</nickname>
<value>18.282</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pb208zPb204</nickname>
<value>38.54</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pb207zPb204</nickname>
<value>15.577</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
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</acquisition>
</acquisitions>
place quantity
ISEI/main/PML-stone-room-111/--/--/A working box for noble-gas analysis 6 months
2019-11-18 15:23 2020-05-16 21:05
description:
ISEI/main/PML-stone-room-111/shelf 2/A working box for noble-gas analysis about 4 years
2015-11-05 14:00 2019-11-18 15:23
description: