pub

IGSN: IEDRM00FL
place: N42°4′55.9″, E143°2′29.4″ more
classification: plutonic:ultramafic
physical-form: aliquot
quantity (kg): 3.405
description: This spinel harzburgite was collected by Eizo in 2000 from Horoman peridotite complex. Initial work was done by M. Tanimoto.
modified at 2020-05-12

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. Lead isotope compositions of natural rock samples < 20200210145025-717332 > in Kuritani, Takeshi & Nakamura, E. (2003)refreshed at 2020-07-30

1: JB-3 powder 2: 0901-3

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

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{20090610090431213.sanjeewa,
 author={{0901-3}},
 title={Aliquot with quantity 3.405 kg at \nolinkurl{/ISEI/stone storage/Room A/1F/G/5/Horoman 2000a/}},
 journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20090610090431213.sanjeewa}{DREAM}},
 volume={20},
 pages={20090610090431213.sanjeewa},
 year={2009},
 url={http://dream.misasa.okayama-u.ac.jp/?q=20090610090431213.sanjeewa},
}

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    <name>0901-3</name>
    <device>XRF PANalytical PW2400</device>
    <technique>XRF procedures of Takei (2002)</technique>
    <operator>Sanjeewa</operator>
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      <longitude>143.0415</longitude>
      <latitude>42.0821944444444</latitude>
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      <analysis>
        <nickname>FeOT</nickname>
        <value>8.14</value>
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  <acquisition>
    <global_id>20181003120021-506043</global_id>
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    <sample_global_id>20090610090431213.sanjeewa</sample_global_id>
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      <analysis>
        <nickname>B</nickname>
        <value>1.02</value>
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      <analysis>
        <nickname>Zr</nickname>
        <value>0.06</value>
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      <analysis>
        <nickname>Hf</nickname>
        <value>0.003</value>
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      <analysis>
        <nickname>Nb</nickname>
        <value>0.01</value>
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      <analysis>
        <nickname>Ta</nickname>
        <value>0.001</value>
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  <acquisition>
    <global_id>20181002155140-552576</global_id>
    <name>0901-3</name>
    <device>XRF PANalytical PW2400</device>
    <technique>XRF procedures of Takei (2002)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090610090431213.sanjeewa</sample_global_id>
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      <latitude>42.0821944444444</latitude>
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    <chemistries>
      <analysis>
        <nickname>SiO2</nickname>
        <value>42.9</value>
        <unit>%</unit>
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      <analysis>
        <nickname>TiO2</nickname>
        <value>0.01</value>
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      <analysis>
        <nickname>Al2O3</nickname>
        <value>0.63</value>
        <unit>%</unit>
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      <analysis>
        <nickname>Cr2O3</nickname>
        <value>0.45</value>
        <unit>%</unit>
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      <analysis>
        <nickname>FeO</nickname>
        <value>8.14</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
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      <analysis>
        <nickname>MnO</nickname>
        <value>0.13</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MgO</nickname>
        <value>46.73</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>NiO</nickname>
        <value>0.34</value>
        <unit>%</unit>
        <uncertainty/>
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        <info/>
      </analysis>
      <analysis>
        <nickname>CaO</nickname>
        <value>0.41</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>K2O</nickname>
        <value>0.004</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>P2O5</nickname>
        <value>0.002</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>LOI</nickname>
        <value>0.75</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>total</nickname>
        <value>100.5</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
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  </acquisition>
  <acquisition>
    <global_id>20181003120545-602479</global_id>
    <name>0901-3</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>20090610090431213.sanjeewa</sample_global_id>
    <sample_name>0901-3</sample_name>
    <description/>
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      <global_id>20160517143722-385941</global_id>
      <name>locality of 0901-3</name>
      <longitude>143.0415</longitude>
      <latitude>42.0821944444444</latitude>
      <elevation/>
      <description/>
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    <chemistries>
      <analysis>
        <nickname>Li</nickname>
        <value>1.36</value>
        <unit>ppm</unit>
        <uncertainty/>
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      <analysis>
        <nickname>Rb</nickname>
        <value>0.03</value>
        <unit>ppm</unit>
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        <label/>
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      <analysis>
        <nickname>Sr</nickname>
        <value>0.17</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Y</nickname>
        <value>0.02</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Cs</nickname>
        <value>0.02</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ba</nickname>
        <value>0.11</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>La</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Ce</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
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      <analysis>
        <nickname>Pr</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
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      </analysis>
      <analysis>
        <nickname>Nd</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
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      </analysis>
      <analysis>
        <nickname>Sm</nickname>
        <value>0.003</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>0.004</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tb</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Dy</nickname>
        <value>0.004</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ho</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Er</nickname>
        <value>0.004</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tm</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Yb</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Lu</nickname>
        <value>0.002</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Pb</nickname>
        <value>0.022</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Th</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>U</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
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  </acquisition>
  <acquisition>
    <global_id>20200210145120-246197</global_id>
    <name>Horo0901-3_Pb</name>
    <device>TIMS Thermo-Fisher MAT261</device>
    <technique>TIMS with double spike correction</technique>
    <operator>Kuritani</operator>
    <sample_global_id>20090610090431213.sanjeewa</sample_global_id>
    <sample_name>0901-3</sample_name>
    <description></description>
    <place>
      <global_id>20160517143722-385941</global_id>
      <name>locality of 0901-3</name>
      <longitude>143.0415</longitude>
      <latitude>42.0821944444444</latitude>
      <elevation/>
      <description/>
    </place>
    <chemistries>
      <analysis>
        <nickname>Pb207zPb204</nickname>
        <value>15.519</value>
        <unit></unit>
        <uncertainty>0.011</uncertainty>
        <label></label>
        <info></info>
      </analysis>
      <analysis>
        <nickname>Pb206zPb204</nickname>
        <value>18.213</value>
        <unit></unit>
        <uncertainty>0.008</uncertainty>
        <label></label>
        <info></info>
      </analysis>
      <analysis>
        <nickname>Pb208zPb204</nickname>
        <value>38.151</value>
        <unit></unit>
        <uncertainty>0.021</uncertainty>
        <label></label>
        <info></info>
      </analysis>
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</acquisitions>

name

physical-form

quantity

0901-3 pub

powder

20090618092635526.sanjeewa

0901-3 pub

20180202131714-330886

place quantity

ISEI/stone storage/Room A/1F/G/--/Horoman 2000a 7 months

2021-01-04 14:51 2021-08-07 19:49

description:

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

2015-12-15 10:06 2021-01-04 14:51

description:

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

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

description:

ISEI/main/127/Horoman 2000a 9 minutes

2015-11-06 17:23 2015-11-06 17:32

description:

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

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

description:

name	device	global-id
0901-3 pub 1	XRF PANalytical PW2400	20181024115609-240242
0901-3 pub 5	Q-ICPMS Agilent 7500cs	20181003120021-506043
0901-3 pub 13	XRF PANalytical PW2400	20181002155140-552576
0901-3 pub 23	Q-ICPMS Agilent 7500cs	20181003120545-602479
Horo0901-3_Pb pub 3	TIMS Thermo-Fisher MAT261	20200210145120-246197
0901-3 pub 1 on 0901-3 pub	Q-ICPMS Agilent 7500cs	20181210102507-089587
0901-3 pub 1 on 0901-3 pub	HR-ICPMS Finningan, Element	20181210105132-540891
0901-3 pub 1 on 0901-3 pub	Thermo Scientific MAT253	20181211105611-601949
0901-3 pub 1 on 0901-3 pub	TIMS Finnigan MAT261, MAT262 and Triton TI	20181211111329-447783
0901-3 pub 1 on 0901-3 pub	Q-ICPMS Agilent 7500cs	20181212104337-193615
0901-3 pub 3 on 0901-3 pub	TIMS Finnigan MAT261, MAT262 and Triton TI	20181210113352-889420
0901-3 pub 1 on 0901-3 pub	Q-ICPMS Agilent 7500cs	20181130100645-730522
0901-3 pub 2 on 0901-3 pub	MC-ICP-MS Finnigan, Neptune	20181211102803-994735
0901-3 pub 1 on 0901-3 pub	MC-ICP-MS Finnigan, Neptune	20181211111538-472152
0901-3 pub 2 on 0901-3 pub	Thermo Scientific MAT253	20181130122357-997590

	name		global-id
	Kuritani, Takeshi & Nakamura, E. (2003) Highly precise and accurate isotope analysis of small amounts of Pb using 205Pb-204Pb and 207Pb-204Pb, two double spikes, Journal of Analytical and Atomic Spectrometry, 18, 1464-1470, doi:10.1039/B310294G . Table 3. Lead isotope compositions of natural rock samples		20091114120415001.hkitagawa
	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 1. Major element compositions of the Horoman peridotites		20091214105156539.sanjeewa
	Malaviarachchi et al. (2010) Melt-peridotite reactions and fluid metasomatism in the upper mantle, revealed from the geochemistry of peridotite and gabbro from the Horoman peridotite massif, Japan, Journal of Petrology, 51, 1417-1445, doi:10.1093/petrology/egq024.		20150914192726-611012

		name		spots	global-id
		0901-3.JPG pub		0	20090610090433735.sanjeewa