pub

IGSN: IEDRM00FS
physical-form: aliquot
quantity (g): 30.19
description: This plagioclase lherzolite was collected by Eizo in 2000 (a drilled core sample). Leave 20090609091553892.sanjeewa on 2015-10-15.; Leave 20111021140541-639-676 on 2015-10-16.
modified at 2019-06-18

Table 1. Major element compositions of the Horoman peridotites < 20181002155357-035338 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2022-06-25

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 1. Mineral modal compositions of the Horoman samples < 20181011122657-794350 > in Malaviarachchi et al. (2010)refreshed at 2022-06-25

1: 0901-4 2: 0902-2 3: 0902-8 4: 0902-8a 5: 0902-8b 6: 0902-8c 7: 0904-1 8: 0901-2 9: 0902-3 10: HR+55 11: HR+20 12: HR+12 13: HR+0 14: HR-37 15: HR-50 16: HR-60 17: HR-70 18: HR-90 19: HR+5 20: HR-10 21: HR-20 22: HR-30 23: HR-40 24: HR-80

(a) EPMA on EPMA JEOL JXA 8500 system

Table 2. Trace element compositions of the Horoman samples < 20181003120730-255298 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2022-06-23

(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 2022-06-25

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 4. Nd and Hf isotopic compositions of the Horoman samples < 20181004140110-522374 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2022-06-25

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: HR+55 16: HR+20 17: HR+12 18: HR+0 19: HR-37 20: HR-50 21: HR-60 22: HR-70 23: HR-90 24: HR+5

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

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

Table 7. Sr isotopic compositions of the Horoman samples < 20181001151020-495322 > in Malaviarachchi et al. (2010)refreshed at 2022-06-21

1: HR+55 2: HR+20 3: HR+12 4: HR+0 5: HR-37 6: HR-50 7: HR-60 8: HR-70 9: HR-90 10: HR+5 11: HR-10 12: HR-20 13: HR-30 14: HR-40 15: HR-80

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

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{20090611091850678.sanjeewa,
 author={{HR+20}},
 title={Aliquot with quantity 30.19 g at \nolinkurl{/ISEI/stone storage/Room A/1F/G/7/Horoman 2010A/}},
 journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20090611091850678.sanjeewa}{DREAM}},
 volume={19},
 pages={20090611091850678.sanjeewa},
 year={2009},
 url={http://dream.misasa.okayama-u.ac.jp/?q=20090611091850678.sanjeewa},
}

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        <nickname>CaO</nickname>
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      <analysis>
        <nickname>Na2O</nickname>
        <value>0.19</value>
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      <analysis>
        <nickname>K2O</nickname>
        <value>0.004</value>
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        <nickname>P2O5</nickname>
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        <nickname>LOI</nickname>
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        <nickname>total</nickname>
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    <global_id>20181003120547-859900</global_id>
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    <sample_global_id>20090611091850678.sanjeewa</sample_global_id>
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      <analysis>
        <nickname>Li</nickname>
        <value>1.78</value>
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      <analysis>
        <nickname>Rb</nickname>
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      <analysis>
        <nickname>Sr</nickname>
        <value>10.2</value>
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        <nickname>Y</nickname>
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        <value>0.0001</value>
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        <nickname>Ba</nickname>
        <value>0.23</value>
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        <nickname>La</nickname>
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        <nickname>Ce</nickname>
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        <nickname>Nd</nickname>
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        <nickname>Sm</nickname>
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        <unit>ppm</unit>
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        <nickname>Eu</nickname>
        <value>0.07</value>
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        <nickname>Tb</nickname>
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        <nickname>Dy</nickname>
        <value>0.39</value>
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      <analysis>
        <nickname>Ho</nickname>
        <value>0.09</value>
        <unit>ppm</unit>
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      <analysis>
        <nickname>Er</nickname>
        <value>0.26</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Tm</nickname>
        <value>0.04</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Yb</nickname>
        <value>0.26</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Lu</nickname>
        <value>0.04</value>
        <unit>ppm</unit>
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        <label/>
        <info/>
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      <analysis>
        <nickname>Pb</nickname>
        <value>0.25</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
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        <nickname>Th</nickname>
        <value>0.003</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
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        <nickname>U</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
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      <analysis>
        <nickname>UzPb</nickname>
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        <nickname>ThzPb</nickname>
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        <nickname>Pb206zPb204</nickname>
        <value>16.548</value>
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        <nickname>Pb207zPb204</nickname>
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        <nickname>Pb208zPb204</nickname>
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        <nickname>Sr</nickname>
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        <nickname>Sr87zSr86</nickname>
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        <nickname>Lu</nickname>
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        <nickname>Hf176zHf177</nickname>
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        <nickname>Lu176zHf177</nickname>
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        <nickname>eHf</nickname>
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      <analysis>
        <nickname>Sm</nickname>
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      <analysis>
        <nickname>Nd143zNd144</nickname>
        <value>0.513684</value>
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        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Sm147zNd144</nickname>
        <value>0.265</value>
        <unit></unit>
        <uncertainty/>
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      <analysis>
        <nickname>eNd</nickname>
        <value>20.2</value>
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        <uncertainty/>
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      <analysis>
        <nickname>modeOfCpx</nickname>
        <value>8.1</value>
        <unit>%</unit>
        <uncertainty/>
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      <analysis>
        <nickname>modeOfOpx</nickname>
        <value>24.5</value>
        <unit>%</unit>
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      <analysis>
        <nickname>modeOfOl</nickname>
        <value>59.7</value>
        <unit>%</unit>
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      <analysis>
        <nickname>modeOfPl</nickname>
        <value>6.4</value>
        <unit>%</unit>
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        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>modeOfSpl</nickname>
        <value>1.3</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
</acquisitions>

name

physical-form

quantity

HR+20 pub

thin section

20120203094949-644-105

HR+20 pub

powder

20130411085053-198895

HR+20 pub

20180202134335-558047

place quantity

ISEI/stone storage/Room A/1F/G/--/Horoman 2010A over 1 year

2021-01-04 14:54 2022-07-31 03:32

description:

ISEI/main/--/C/4/Horoman 2010A about 5 years

2015-12-15 10:06 2021-01-04 14:54

description:

ISEI/main/--/C/5/Horoman 2010A 1 minute

2015-12-15 10:04 2015-12-15 10:06

description:

ISEI/main/--/C/6/5/Horoman 2010A less than a minute

2015-12-15 10:04 2015-12-15 10:04

description:

ISEI/main/--/C/5/Horoman 2010A about 1 month

2015-11-06 17:22 2015-12-15 10:04

description:

ISEI/main/--/Horoman 2010A 1 day

2015-11-05 14:00 2015-11-06 17:22

description:

name	device	global-id
HR +20 pub 1	XRF PANalytical PW2400	20181024115609-081451
HR +20 pub 5	Q-ICPMS Agilent 7500cs	20181003120021-026739
HR +20 pub 14	XRF PANalytical PW2400	20181002155141-992563
HR +20 pub 23	Q-ICPMS Agilent 7500cs	20181003120547-859900
HR +20 pub 5	MC-ICP-MS Finnigan, Neptune	20181004103530-828962
HR+20 pub 4	TIMS Finnigan MAT261, MAT262 and Triton TI	20181004103827-780861
HR +20 pub 5	MC-ICP-MS Finnigan, Neptune	20181004135957-866943
HR +20 pub 5	TIMS Finnigan MAT261, MAT262 and Triton TI	20181004140012-664890
HR +20 pub 5	EPMA JEOL JXA 8500 system	20181011122911-326793
HR+20 pub 7 on HR+20 pub	EPMA JEOL JXA-8800R	20181128124258-570157
HR+20 pub 1 on HR+20 pub	Q-ICPMS Agilent 7500cs	20181210102508-196472
HR+20 pub 1 on HR+20 pub	HR-ICPMS Finningan, Element	20181210105132-282158
HR+20 pub 1 on HR+20 pub	Thermo Scientific MAT253	20181211105612-249165
HR+20 pub 1 on HR+20 pub	Q-ICPMS Agilent 7500cs	20181212104337-144166
HR+20 pub 3 on HR+20 pub	TIMS Finnigan MAT261, MAT262 and Triton TI	20181210113352-748742
HR+20 pub 2 on HR+20 pub	Q-ICPMS Agilent 7500cs	20181130100646-181330
HR+20 pub 2 on HR+20 pub	MC-ICP-MS Finnigan, Neptune	20181211102803-290749
HR+20 pub 2 on HR+20 pub	Thermo Scientific MAT253	20181130122358-269652

	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 1. Major element compositions of the Horoman peridotites Table 3. Pb isotopic composition of the Horoman samples Table 4. Nd and Hf isotopic compositions of the Horoman samples		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. Table 7. Sr isotopic compositions of the Horoman samples Table 1. Mineral modal compositions of the Horoman samples		20150914192726-611012

		name		spots	global-id
		HR_20.JPG pub		0	20090611091852569.sanjeewa