Determination of Re, Os, Ir, Ru, Pt, Pd Mass Fractions and Os-187/Os-188 Ratios of Organic-Rich Geological Reference Materials

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Determination of Re, Os, Ir, Ru, Pt, Pd Mass Fractions and Os-187/Os-188 Ratios of Organic-Rich Geological Reference Materials. / Wang, Mengjie; Chu, Zhuyin; Meisel, Thomas C. et al.
In: Geostandards and Geoanalytical Research, Vol. 46.2022, No. 2, 11.04.2022, p. 333-349.

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@article{b918941206dd4d9ea207d8f374064f1f,
title = "Determination of Re, Os, Ir, Ru, Pt, Pd Mass Fractions and Os-187/Os-188 Ratios of Organic-Rich Geological Reference Materials",
abstract = "At present, reported data for Re-PGE mass fractions (in particular) and 187Os/188Os isotope ratios of organic-rich reference materials (RMs) are rare, hampering the comparison of data quality between different laboratories. In this study, we measured the Re-PGE (Os, Ir, Ru, Pt and Pd) mass fractions, as well as 187Os/188Os isotope ratios of five shale RMs, including USGS SGR-1b (oil shale), SBC-1 (marine shale), SCo-2 (silty marine shale), ShTX-1 (calcareous organic-rich shale) and ShCX-1 (calcareous shale), and one oil RM, NIST RM 8505. The results show that the five shale RMs have similar upper continental crust-normalised PGE-Re patterns and are generally homogeneous in Re-PGE mass fractions and 187Os/188Os isotope ratios at test portions of 0.2–0.5 g, and thus can be used as matrix-matched RMs for Re-Os and PGE of shale samples. The oil RM NIST 8505 and its asphaltene separates are also roughly homogeneous in Re-PGE mass fractions and 187Os/188Os isotope ratios at test portions of 0.1–0.3 g and can potentially be used as an oil RM for Re-Os and PGE.",
author = "Mengjie Wang and Zhuyin Chu and Meisel, {Thomas C.} and Jinghui Guo",
note = "Publisher Copyright: {\textcopyright} 2022 The Authors. Geostandards and Geoanalytical Research {\textcopyright} 2022 International Association of Geoanalysts.",
year = "2022",
month = apr,
day = "11",
doi = "10.1111/ggr.12423",
language = "English",
volume = "46.2022",
pages = "333--349",
journal = "Geostandards and Geoanalytical Research",
issn = "1639-4488",
publisher = "Wiley-Blackwell, USA",
number = "2",

}

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TY - JOUR

T1 - Determination of Re, Os, Ir, Ru, Pt, Pd Mass Fractions and Os-187/Os-188 Ratios of Organic-Rich Geological Reference Materials

AU - Wang, Mengjie

AU - Chu, Zhuyin

AU - Meisel, Thomas C.

AU - Guo, Jinghui

N1 - Publisher Copyright: © 2022 The Authors. Geostandards and Geoanalytical Research © 2022 International Association of Geoanalysts.

PY - 2022/4/11

Y1 - 2022/4/11

N2 - At present, reported data for Re-PGE mass fractions (in particular) and 187Os/188Os isotope ratios of organic-rich reference materials (RMs) are rare, hampering the comparison of data quality between different laboratories. In this study, we measured the Re-PGE (Os, Ir, Ru, Pt and Pd) mass fractions, as well as 187Os/188Os isotope ratios of five shale RMs, including USGS SGR-1b (oil shale), SBC-1 (marine shale), SCo-2 (silty marine shale), ShTX-1 (calcareous organic-rich shale) and ShCX-1 (calcareous shale), and one oil RM, NIST RM 8505. The results show that the five shale RMs have similar upper continental crust-normalised PGE-Re patterns and are generally homogeneous in Re-PGE mass fractions and 187Os/188Os isotope ratios at test portions of 0.2–0.5 g, and thus can be used as matrix-matched RMs for Re-Os and PGE of shale samples. The oil RM NIST 8505 and its asphaltene separates are also roughly homogeneous in Re-PGE mass fractions and 187Os/188Os isotope ratios at test portions of 0.1–0.3 g and can potentially be used as an oil RM for Re-Os and PGE.

AB - At present, reported data for Re-PGE mass fractions (in particular) and 187Os/188Os isotope ratios of organic-rich reference materials (RMs) are rare, hampering the comparison of data quality between different laboratories. In this study, we measured the Re-PGE (Os, Ir, Ru, Pt and Pd) mass fractions, as well as 187Os/188Os isotope ratios of five shale RMs, including USGS SGR-1b (oil shale), SBC-1 (marine shale), SCo-2 (silty marine shale), ShTX-1 (calcareous organic-rich shale) and ShCX-1 (calcareous shale), and one oil RM, NIST RM 8505. The results show that the five shale RMs have similar upper continental crust-normalised PGE-Re patterns and are generally homogeneous in Re-PGE mass fractions and 187Os/188Os isotope ratios at test portions of 0.2–0.5 g, and thus can be used as matrix-matched RMs for Re-Os and PGE of shale samples. The oil RM NIST 8505 and its asphaltene separates are also roughly homogeneous in Re-PGE mass fractions and 187Os/188Os isotope ratios at test portions of 0.1–0.3 g and can potentially be used as an oil RM for Re-Os and PGE.

UR - http://www.scopus.com/inward/record.url?scp=85127979063&partnerID=8YFLogxK

U2 - 10.1111/ggr.12423

DO - 10.1111/ggr.12423

M3 - Article

VL - 46.2022

SP - 333

EP - 349

JO - Geostandards and Geoanalytical Research

JF - Geostandards and Geoanalytical Research

SN - 1639-4488

IS - 2

ER -