Thermal metamorphism of CM chondrites: A dehydroxylation‐based peak‐temperature thermometer and implications for sample return from asteroids Ryugu and Bennu-Reference-Cited by-同舟云学术

Thermal metamorphism of CM chondrites: A dehydroxylation‐based peak‐temperature thermometer and implications for sample return from asteroids Ryugu and Bennu

Published:2021-03 Issue:3 Volume:56 Page:546-585
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Velbel Michael A.¹²^ORCID,Zolensky Michael E.³^ORCID

Affiliation:

1. Department of Earth and Environmental Sciences Michigan State University 288 Farm Lane, Room 207, Natural Sciences Building East Lansing Michigan 48824–1115 USA

2. Division of Meteorites Department of Mineral Sciences National Museum of Natural History Smithsonian Institution Washington District of Columbia 20013–7012 USA

3. X12 Astromaterials Research and Exploration Science NASA Johnson Space Center Houston Texas 77058 USA

Funder

Michigan Space Grant Consortium

National Aeronautics and Space Administration

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.13636

Reference219 articles.

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2. Mineralogical evidence of heating events in Antarctic carbonaceous chondrites, Y‐86720 and Y‐82162;Akai J.;Proceedings of the NIPR Symposium on Antarctic Meteorites,1990

3. T‐T‐T diagram of serpentine and saponite, and estimation of metamorphic heating degree of Antarctic carbonaceous chondrites;Akai J.;Proceedings of the NIPR Symposium on Antarctic Meteorites,1992

4. The Provenances of Asteroids, and Their Contributions to the Volatile Inventories of the Terrestrial Planets

5. The classification of CM and CR chondrites using bulk H, C and N abundances and isotopic compositions

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