pub

IGSN: IEDRM00FG
physical-form: aliquot
quantity (kg): 3.76
description: This harzburgite was collected by Eizo in 2000. Initial work was done by M. Tanimoto. Leave Horoman 2000a <20090609091553892.sanjeewa> and enter Horoman 2000w <20151106110332-840033> on 2015-11-06.
modified at 2019-06-24

Table 1. Major element compositions of the Horoman peridotites < 20181002155357-035338 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2021-06-02

1: 0901-4 2: 0901-4a 3: 0901-4b 4: 0901-4c 5: 0902-2 6: 0902-2a 7: 0902-8 8: 0902-8a 9: 0902-8b 10: 0902-8c 11: 0904-1 12: 0904-1a 13: 0904-1b 14: 0904-1c 15: 0901-1 16: 0902-1 17: 0904-2 18: 0901-2 19: 0901-3 20: 0902-3 21: 0902-10 22: 0903-13 23: HR+55 24: HR+20 25: HR+12 26: HR+0 27: HR-37 28: HR-50 29: HR-60 30: HR-70 31: HR-90 32: HR+5

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

Table 2. Trace element compositions of the Horoman samples < 20181003120730-255298 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2021-06-02

(a) Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006) on Q-ICPMS Agilent 7500cs

Table 3. Pb isotopic composition of the Horoman samples < 20181003143947-011557 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2021-06-02

1: 0901-4 2: 0901-4a 3: 0901-4b 4: 0901-4c 5: 0902-2 6: 0902-2a 7: 0902-8 8: 0902-8a 9: 0902-8b 10: 0902-8c 11: 0904-1 12: 0904-1a 13: 0904-1b 14: 0904-1c 15: 0901-1 16: 0904-2 17: 0901-2 18: 0902-3 19: 0902-10 20: 0903-13 21: HR+55 22: HR+20 23: HR+12 24: HR+0 25: HR-37 26: HR-50 27: HR-60 28: HR-70 29: HR-90 30: HR+5

(a) Pb isotopes_procedures of Makishima et al., (2007) on MC-ICP-MS Finnigan, Neptune

Table S1 . Modal abundances of minerals in the Horoman peridotites < 20181128103409-089107 > in Lalindra V. Ranaweera et al. (2018)refreshed at 2020-07-30

1: 0901-4 2: 0901-4a 3: 0901-4b 4: 0901-4c ts 5: 0902-2 6: 0902-2a 7: 0902-8 8: 0902-8a 9: 0902-8b 10: 0902-8c 11: 0904-1 12: 0904-1a 13: 0904-1b 14: 0904-1c 15: 0901-1 16: 0902-1 17: 0904-2 18: 0901-2 19: 0901-3 20: 0902-3 21: 0902-10 22: 0903-13 23: HR+55 24: HR+20 25: HR+12 26: HR+0 27: HR-37 28: HR-50 29: HR-60 30: HR-70 31: HR-90 32: HR+5

(a) EPMA on EPMA JEOL JXA-8800R

Table S2. Elemental and isotope abundances of the Horoman peridotites < 20181211095123-164197 > in Lalindra V. Ranaweera et al. (2018)refreshed at 2020-07-30

(a) Ion chromatography with pyrohydrolysis on Q-ICPMS Agilent 7500cs

(b) IRMS with TCEA on Thermo Scientific MAT253

(d) oxidation of S into sulfate (Makishima et al., 2001) on HR-ICPMS Finningan, Element

(e) Sr isotopes_procedures of Yoshikawa and Nakamura (1993) on TIMS Finnigan MAT261, MAT262 and Triton TI

(f) Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006) on Q-ICPMS Agilent 7500cs

(g) Pb=2*Pb/(Ce+Pr) on Q-ICPMS Agilent 7500cs

(h) Li isotopes_procedures of Moriguti and Nakamura (1998) on MC-ICP-MS Finnigan, Neptune

(i) IRMS with LF on Thermo Scientific MAT253

(j) Pb isotopes_procedures of Makishima et al., (2007) on MC-ICP-MS Finnigan, Neptune

(k) TIMS with double spike correction on TIMS Thermo-Fisher MAT261

(l) Nd isotopes_procedures of Nakamura et al. (1991, 2003) on TIMS Finnigan MAT261, MAT262 and Triton TI

(m) Hf isotopes_procedures of Lu et al. (2007) on MC-ICP-MS Finnigan, Neptune

@article{20090610090449371.sanjeewa,
 author={{0903-13}},
 title={Aliquot with quantity 3.76 kg at \nolinkurl{/ISEI/stone storage/Room A/1F/F/2/Horoman 2000w/}},
 journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20090610090449371.sanjeewa}{DREAM}},
 volume={19},
 pages={20090610090449371.sanjeewa},
 year={2009},
 url={http://dream.misasa.okayama-u.ac.jp/?q=20090610090449371.sanjeewa},
}

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    <global_id>20181024115609-792369</global_id>
    <name>0903-13</name>
    <device>XRF PANalytical PW2400</device>
    <technique>XRF procedures of Takei (2002)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090610090449371.sanjeewa</sample_global_id>
    <sample_name>0903-13</sample_name>
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      <analysis>
        <nickname>FeOT</nickname>
        <value>8.62</value>
        <unit>%</unit>
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  </acquisition>
  <acquisition>
    <global_id>20181003120021-132332</global_id>
    <name>0903-13</name>
    <device>Q-ICPMS Agilent 7500cs</device>
    <technique>Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090610090449371.sanjeewa</sample_global_id>
    <sample_name>0903-13</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>B</nickname>
        <value>2.65</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Zr</nickname>
        <value>0.07</value>
        <unit>ppm</unit>
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      </analysis>
      <analysis>
        <nickname>Hf</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
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      </analysis>
      <analysis>
        <nickname>Nb</nickname>
        <value>0.04</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Ta</nickname>
        <value>0.003</value>
        <unit>ppm</unit>
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  </acquisition>
  <acquisition>
    <global_id>20181002155140-808965</global_id>
    <name>0903-13</name>
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    <operator>Sanjeewa</operator>
    <sample_global_id>20090610090449371.sanjeewa</sample_global_id>
    <sample_name>0903-13</sample_name>
    <description/>
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      <analysis>
        <nickname>SiO2</nickname>
        <value>43.7</value>
        <unit>%</unit>
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      <analysis>
        <nickname>TiO2</nickname>
        <value>0.01</value>
        <unit>%</unit>
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      <analysis>
        <nickname>Al2O3</nickname>
        <value>0.9</value>
        <unit>%</unit>
        <uncertainty/>
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      </analysis>
      <analysis>
        <nickname>Cr2O3</nickname>
        <value>0.38</value>
        <unit>%</unit>
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      <analysis>
        <nickname>FeO</nickname>
        <value>8.62</value>
        <unit>%</unit>
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      <analysis>
        <nickname>MnO</nickname>
        <value>0.13</value>
        <unit>%</unit>
        <uncertainty/>
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      </analysis>
      <analysis>
        <nickname>MgO</nickname>
        <value>45.42</value>
        <unit>%</unit>
        <uncertainty/>
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      </analysis>
      <analysis>
        <nickname>NiO</nickname>
        <value>0.33</value>
        <unit>%</unit>
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      </analysis>
      <analysis>
        <nickname>CaO</nickname>
        <value>0.86</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>K2O</nickname>
        <value>0.006</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>P2O5</nickname>
        <value>0.001</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>LOI</nickname>
        <value>0.07</value>
        <unit>%</unit>
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      <analysis>
        <nickname>total</nickname>
        <value>100.4</value>
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  <acquisition>
    <global_id>20181003120546-415476</global_id>
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    <device>Q-ICPMS Agilent 7500cs</device>
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    <operator>Sanjeewa</operator>
    <sample_global_id>20090610090449371.sanjeewa</sample_global_id>
    <sample_name>0903-13</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>Li</nickname>
        <value>1.52</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Rb</nickname>
        <value>0.04</value>
        <unit>ppm</unit>
        <uncertainty/>
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      <analysis>
        <nickname>Sr</nickname>
        <value>0.22</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Y</nickname>
        <value>0.03</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
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      <analysis>
        <nickname>Cs</nickname>
        <value>0.003</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ba</nickname>
        <value>0.17</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>La</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ce</nickname>
        <value>0.02</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Pr</nickname>
        <value>0.004</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nd</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sm</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Eu</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Gd</nickname>
        <value>0.002</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tb</nickname>
        <value>0.0005</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Dy</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ho</nickname>
        <value>0.002</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Er</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tm</nickname>
        <value>0.002</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Yb</nickname>
        <value>0.02</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Lu</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pb</nickname>
        <value>0.034</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Th</nickname>
        <value>0.003</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>U</nickname>
        <value>0.002</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
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  <acquisition>
    <global_id>20181004103530-531230</global_id>
    <name>0903-13</name>
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    <technique>Pb isotopes_procedures of Makishima et al., (2007)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090610090449371.sanjeewa</sample_global_id>
    <sample_name>0903-13</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>UzPb</nickname>
        <value>0.101</value>
        <unit></unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>ThzPb</nickname>
        <value>0.134</value>
        <unit></unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Pb206zPb204</nickname>
        <value>18.521</value>
        <unit></unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Pb207zPb204</nickname>
        <value>15.605</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pb208zPb204</nickname>
        <value>38.543</value>
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name

physical-form

quantity

0903-13 pub

powder

20090618092844297.sanjeewa

0903-13 pub

thin section

20091002091814729.sanjeewa

0903-13 pub

20180202134026-173295

place quantity

ISEI/stone storage/Room A/1F/F/--/Horoman 2000w 8 months

2021-01-04 14:27 2021-08-26 23:18

description:

ISEI/main/127/C/3/Horoman 2000w about 5 years

2015-12-15 10:06 2021-01-04 14:27

description:

ISEI/main/127/B/1/Horoman 2000w about 1 month

2015-11-06 17:32 2015-12-15 10:06

description:

ISEI/main/127/Horoman 2000w 1 minute

2015-11-06 17:31 2015-11-06 17:32

description:

ISEI/main/127/Horoman 2000a 8 minutes

2015-11-06 17:23 2015-11-06 17:31

description:

ISEI/main/--/Horoman 2000a 1 day

2015-11-05 14:00 2015-11-06 17:23

description:

name	device	global-id
0903-13 pub 1	XRF PANalytical PW2400	20181024115609-792369
0903-13 pub 5	Q-ICPMS Agilent 7500cs	20181003120021-132332
0903-13 pub 13	XRF PANalytical PW2400	20181002155140-808965
0903-13 pub 23	Q-ICPMS Agilent 7500cs	20181003120546-415476
0903-13 pub 5	MC-ICP-MS Finnigan, Neptune	20181004103530-531230
0903-13 pub 1 on 0903-13 pub	Q-ICPMS Agilent 7500cs	20181210102508-407281
0903-13 pub 1 on 0903-13 pub	HR-ICPMS Finningan, Element	20181210105132-955284
0903-13 pub 1 on 0903-13 pub	Thermo Scientific MAT253	20181211105611-464055
0903-13 pub 1 on 0903-13 pub	TIMS Finnigan MAT261, MAT262 and Triton TI	20181211111329-916749
0903-13 pub 1 on 0903-13 pub	Q-ICPMS Agilent 7500cs	20181212104337-217336
0903-13 pub 3 on 0903-13 pub	TIMS Finnigan MAT261, MAT262 and Triton TI	20181210113352-360483
0903-13 pub 2 on 0903-13 pub	Q-ICPMS Agilent 7500cs	20181130100646-558131
0903-13 pub 2 on 0903-13 pub	MC-ICP-MS Finnigan, Neptune	20181211102803-314256
0903-13 pub 5 on 0903-13 pub	EPMA JEOL JXA-8800R	20181128124258-327284
0903-13 pub 2 on 0903-13 pub	Thermo Scientific MAT253	20181130122358-577490

	name		global-id
	Lalindra V. Ranaweera et al. (2018) Circa 1 Ga sub-seafloor hydrothermal alteration imprinted on the Horoman peridotite massif, Scientific Reports, 8, doi:10.1038/s41598-018-28219-x. Table S2. Elemental and isotope abundances of the Horoman peridotites Table S1 . Modal abundances of minerals in the Horoman peridotites		20181128101201-565661
	Sanjeewa P. K. Malaviarachchi et al. (2008) Highly unradiogenic lead isotope ratios from the Horoman peridotite in Japan, Nature Geoscience, 1, 859 - 863, doi:10.1038/ngeo363. Table 2. Trace element compositions of the Horoman samples Table 3. Pb isotopic composition of the Horoman samples Table 1. Major element compositions of the Horoman peridotites		20091214105156539.sanjeewa

		name		spots	global-id
		0903-13.JPG pub		0	20090610090451802.sanjeewa