pub

IGSN: IEDRM00O8
classification: volcanic:basaltic
physical-form: hand specimen
quantity (g): 807.35
description: Kutsugata Lava, North Lava, basaltic andesite
modified at 2020-02-13

Table 1. Whole-rock compositions of representative samples < 20190620153525-761634 > in Kuritani et al. (2007)refreshed at 2020-07-30

1: Ta-25 2: Ta-31 3: Kr 28 4: Kr 41 5: KR 9 6: Ta-28 7: Kr 74 8: Kr 72 9: Kr 47

(a) XRF procedures of Takei (2002) on XRF PANalytical PW2400

(b) Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006) on ICPMS Yokogawa PMS2000

(d) Pb isotopes_procedures of Kuritani and Nakamura (2002, 2003) on TIMS Finnigan MAT261, MAT262 and Triton TI

Table 2. U and Th isotopic compositions and concentrations of Rishiri samples < 20190621100851-003231 > in Kuritani et al. (2007)refreshed at 2020-07-30

1: Ta-25U-Th_1 2: Ta-25U-Th_2 3: Ta-31U-Th_1 4: Ta-31U-Th_2 5: Kr 28U-Th_1 6: Kr 28U-Th_2 7: Kr-41U-Th_1 8: Kr-41U-Th_2 9: Kr-9U-Th_1 10: Kr-9U-Th_2 11: Kr 74U-Th_1 12: Kr 74U-Th_2 13: Kr 72U-Th_1 14: Kr 72U-Th_2 15: Kr 47U-Th_1 16: Kr 47U-Th_2 17: Ta-1U-Th_1 18: Ta-1U-Th_2 19: Ta-1U-Th_3 20: Ta-1U-Th_4 21: Ta-1U-Th_5 22: Ta-1U-Th_6 23: Ta-1U-Th_7 24: Ta-1U-Th_8 25: Ta-2U-Th_1 26: Ta-2U-Th_2 27: Ta-2U-Th_3 28: Ta-11U-Th_1 29: Ta-11U-Th_2 30: Ta-11U-Th_3 31: Ta-17U-Th_1 32: Ta-17U-Th_2 33: Ta-17U-Th_3 34: Ta-17U-Th_4 35: Ta-17U-Th_5 36: Ta-28U-Th_1 37: Ta-28U-Th_2 38: Ta-28U-Th_3 39: Ta-28U-Th_4 40: Ta-28U-Th_5 41: Ta-28U-Th_6

(a) U-Series_procedures of Yokoyama et al. (1999, 2001, 2003) on TIMS Thermo-Fisher MAT261

@article{20151130084230-279167,
 author={{Ta-25}},
 title={Hand specimen with quantity 807.35 g at \nolinkurl{/ISEI/stone storage/Room A/2F/A/3/Kuritani 21/}},
 journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20151130084230-279167}{DREAM}},
 volume={20},
 pages={20151130084230-279167},
 year={2015},
 url={http://dream.misasa.okayama-u.ac.jp/?q=20151130084230-279167},
}

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<acquisitions>
  <acquisition>
    <global_id>20190620160217-740035</global_id>
    <name>Ta-25_2007</name>
    <device>XRF PANalytical PW2400</device>
    <technique>XRF procedures of Takei (2002)</technique>
    <operator>Kuritani</operator>
    <sample_global_id>20151130084230-279167</sample_global_id>
    <sample_name>Ta-25</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>SiO2</nickname>
        <value>52.23</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>TiO2</nickname>
        <value>1.44</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Al2O3</nickname>
        <value>17.56</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Fe2O3T</nickname>
        <value>8.96</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MnO</nickname>
        <value>0.16</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MgO</nickname>
        <value>5.43</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>CaO</nickname>
        <value>9.44</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Na2O</nickname>
        <value>4.19</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>K2O</nickname>
        <value>0.61</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>P2O5</nickname>
        <value>0.3</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>LOI</nickname>
        <value>-0.16</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>total</nickname>
        <value>100.16</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Cr</nickname>
        <value>145.0</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ni</nickname>
        <value>54.0</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20190621092556-252261</global_id>
    <name>Ta-25_2007</name>
    <device>TIMS Thermo-Fisher MAT261</device>
    <technique>TIMS with isotope dilution</technique>
    <operator>Kuritani</operator>
    <sample_global_id>20151130084230-279167</sample_global_id>
    <sample_name>Ta-25</sample_name>
    <description></description>
    <chemistries>
      <analysis>
        <nickname>Pb</nickname>
        <value>2.86</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20190621092709-233128</global_id>
    <name>Ta-25</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>20151130084230-279167</sample_global_id>
    <sample_name>Ta-25</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>Pb206zPb204</nickname>
        <value>18.242</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pb207zPb204</nickname>
        <value>15.507</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pb208zPb204</nickname>
        <value>38.101</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20190621091432-412385</global_id>
    <name>Ta-25_2007</name>
    <device>ICPMS Yokogawa PMS2000</device>
    <technique>Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006)</technique>
    <operator>Kuritani</operator>
    <sample_global_id>20151130084230-279167</sample_global_id>
    <sample_name>Ta-25</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>Li</nickname>
        <value>8.25</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>B</nickname>
        <value>3.95</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Rb</nickname>
        <value>14.1</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sr</nickname>
        <value>441.0</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Y</nickname>
        <value>34.4</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Zr</nickname>
        <value>169.0</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nb</nickname>
        <value>4.55</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Cs</nickname>
        <value>0.84</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ba</nickname>
        <value>140.0</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>La</nickname>
        <value>13.4</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ce</nickname>
        <value>33.1</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pr</nickname>
        <value>4.21</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nd</nickname>
        <value>19.0</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sm</nickname>
        <value>4.55</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Eu</nickname>
        <value>1.57</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Gd</nickname>
        <value>4.86</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tb</nickname>
        <value>0.82</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Dy</nickname>
        <value>5.16</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ho</nickname>
        <value>1.13</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Er</nickname>
        <value>3.02</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tm</nickname>
        <value>0.47</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Yb</nickname>
        <value>3.18</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Lu</nickname>
        <value>0.47</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Hf</nickname>
        <value>3.58</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ta</nickname>
        <value>0.35</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
</acquisitions>

name

physical-form

quantity

Ta-25U-Th_1 pub

20190621094316-127365

Ta-25U-Th_2 pub

20190621094316-375618

place quantity

ISEI/stone storage/Room A/2F/A/3/Kuritani 21 8 months

2020-12-25 15:43 2021-08-11 17:42

description:

ISEI/main/127/D/6/Kuritani 21 about 5 years

2015-12-09 10:12 2020-12-25 15:43

description:

ISEI/main/127/D/2/Kuritani 21 9 days

2015-11-30 09:14 2015-12-09 10:12

description:

ISEI/main/127/Kuritani 21 29 minutes

2015-11-30 08:45 2015-11-30 09:14

description:

name	device	global-id
Ta-25_2007 pub 14	XRF PANalytical PW2400	20190620160217-740035
Ta-25_2007 pub 1	TIMS Thermo-Fisher MAT261	20190621092556-252261
Ta-25 pub 3	TIMS Finnigan MAT261, MAT262 and Triton TI	20190621092709-233128
Ta-25_2007 pub 25	ICPMS Yokogawa PMS2000	20190621091432-412385
Ta-25U-Th_1 pub 5 on Ta-25U-Th_1 pub	TIMS Thermo-Fisher MAT261	20190621100737-248924
Ta-25U-Th_2 pub 5 on Ta-25U-Th_2 pub	TIMS Thermo-Fisher MAT261	20190621100737-682020

	name		global-id
	Kuritani et al. (2007) Rates of Thermal and Chemical Evolution of Magmas in a Cooling Magma Chamber: a Chronological and Theoretical Study on Basaltic and Andesitic Lavas from Rishiri Volcano, Japan, J. Petrol., 48, 1295-1319, doi:10.1093/petrology/egm018. Table 1. Whole-rock compositions of representative samples Table 2. U and Th isotopic compositions and concentrations of Rishiri samples		20100403101828129.admin

		name		spots	global-id
		tixhr257428535.jpg pub		0	20151130084907-134258