Large sulfur isotope fractionation in lunar volcanic glasses reveals the magmatic differentiation and degassing of the Moon.


Journal

Science advances
ISSN: 2375-2548
Titre abrégé: Sci Adv
Pays: United States
ID NLM: 101653440

Informations de publication

Date de publication:
Feb 2021
Historique:
received: 23 08 2020
accepted: 08 01 2021
entrez: 25 2 2021
pubmed: 26 2 2021
medline: 26 2 2021
Statut: epublish

Résumé

Sulfur isotope variations in mantle-derived lavas provide important constraints on the evolution of planetary bodies. Here, we report the first in situ measurements of sulfur isotope ratios dissolved in primitive volcanic glasses and olivine-hosted melt inclusions recovered from the Moon by the Apollo 15 and 17 missions. The new data reveal large variations in

Identifiants

pubmed: 33627430
pii: 7/9/eabe4641
doi: 10.1126/sciadv.abe4641
pmc: PMC7904258
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Informations de copyright

Copyright © 2021 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).

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Auteurs

Alberto E Saal (AE)

Department of Earth Environmental and Planetary Sciences, Brown University, Providence, RI 02912, USA. asaal@brown.edu.

Erik H Hauri (EH)

The Earth and Planets Laboratory, Carnegie Institution for Sciences, Washington, DC 20015, USA.

Classifications MeSH