Hydrogen Isotopic Variations in the Shergottites
Hydrogen isotopes in the shergottite Martian meteorites are among the most varied in Mars laboratory samples. By collating results of previous studies on major hydroxyl, deuterium, and H<sub>2</sub>O bearing phases, we provide a compendium of recent measurements in order to elucidate cru...
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MDPI AG
2020-04-01
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Online Access: | https://www.mdpi.com/2076-3263/10/4/148 |
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author | Shuai Wang Sen Hu |
author_facet | Shuai Wang Sen Hu |
author_sort | Shuai Wang |
collection | DOAJ |
description | Hydrogen isotopes in the shergottite Martian meteorites are among the most varied in Mars laboratory samples. By collating results of previous studies on major hydroxyl, deuterium, and H<sub>2</sub>O bearing phases, we provide a compendium of recent measurements in order to elucidate crustal-rock versus mantle-rock processes on Mars. We summarize recent works on volatile and δD measurements in a range of shergottite phases: from melt inclusions, apatite, merrillite, maskelynite, impact melt glass, groundmass glass, and nominal anhydrous minerals. We interpret these observations using an evidence-based approach, considering two particular scenarios: (1) water-rock crustal interactions versus (2) magmatic-based processes. We consider the implications of these measurements and the scope they have for future studies, paying particular attention to future works on H, S, and Cl isotopes in situ, shedding light on the nature of volatiles in the hydrosphere and lithosphere of Mars. |
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issn | 2076-3263 |
language | English |
last_indexed | 2024-03-10T20:24:18Z |
publishDate | 2020-04-01 |
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spelling | doaj.art-87ac9469895643f09e779ba5045d36e92023-11-19T21:55:52ZengMDPI AGGeosciences2076-32632020-04-0110414810.3390/geosciences10040148Hydrogen Isotopic Variations in the ShergottitesShuai Wang0Sen Hu1Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaKey Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaHydrogen isotopes in the shergottite Martian meteorites are among the most varied in Mars laboratory samples. By collating results of previous studies on major hydroxyl, deuterium, and H<sub>2</sub>O bearing phases, we provide a compendium of recent measurements in order to elucidate crustal-rock versus mantle-rock processes on Mars. We summarize recent works on volatile and δD measurements in a range of shergottite phases: from melt inclusions, apatite, merrillite, maskelynite, impact melt glass, groundmass glass, and nominal anhydrous minerals. We interpret these observations using an evidence-based approach, considering two particular scenarios: (1) water-rock crustal interactions versus (2) magmatic-based processes. We consider the implications of these measurements and the scope they have for future studies, paying particular attention to future works on H, S, and Cl isotopes in situ, shedding light on the nature of volatiles in the hydrosphere and lithosphere of Mars.https://www.mdpi.com/2076-3263/10/4/148Marsshergottiteswater-rock interactionhydrogen isotopeswater content |
spellingShingle | Shuai Wang Sen Hu Hydrogen Isotopic Variations in the Shergottites Geosciences Mars shergottites water-rock interaction hydrogen isotopes water content |
title | Hydrogen Isotopic Variations in the Shergottites |
title_full | Hydrogen Isotopic Variations in the Shergottites |
title_fullStr | Hydrogen Isotopic Variations in the Shergottites |
title_full_unstemmed | Hydrogen Isotopic Variations in the Shergottites |
title_short | Hydrogen Isotopic Variations in the Shergottites |
title_sort | hydrogen isotopic variations in the shergottites |
topic | Mars shergottites water-rock interaction hydrogen isotopes water content |
url | https://www.mdpi.com/2076-3263/10/4/148 |
work_keys_str_mv | AT shuaiwang hydrogenisotopicvariationsintheshergottites AT senhu hydrogenisotopicvariationsintheshergottites |