Formation and transformations of Fe-rich serpentines by asteroidal aqueous alteration processes: A nanoscale study of the Murray chondrite-Reference-Cited by-同舟云学术

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Formation and transformations of Fe-rich serpentines by asteroidal aqueous alteration processes: A nanoscale study of the Murray chondrite

Published:2015-06 Issue: Volume:158 Page:162-178
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Elmaleh Agnès,Bourdelle Franck,Caste Florent,Benzerara Karim,Leroux Hugues,Devouard Bertrand

Funder

ANR

Région Ile de France

Conseil Regional du Nord-Pas de Calais

ERDF

NSERC

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference79 articles.

1. Subsurface structure of a submarine hydrothermal system in ocean crust formed at the East Pacific Rise, ODP/IODP Site 1256;Alt;Geochem. Geophys. Geosyst.,2010

2. Deuterium enrichments in chondritic macromolecular material – implications for the origin and evolution of organics, water and asteroids;Alexander;Geochim. Cosmochim. Acta,2010

3. Dynamic control on serpentine crystallization in veins: Constraints on hydration processes in oceanic peridotites

4. Polysomatism, polytypism, defect microstructures and reaction mechanisms in regularly and randomly interstratified serpentine and chlorite;Banfield;Contrib. Mineral. Petrol.,1994

5. The redox state of iron in the matrix of CI, CM and metamorphosed CM chondrites by XANES spectroscopy;Beck;Geochim. Cosmochim. Acta,2012

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5. Complex diagnostics of ordinary chondrites Markovka, Polujamki, Sayh al Uhaymir 001, Dhofar 020, and Jiddat al Harasis 055 by X‐ray techniques and Mössbauer spectroscopy;Meteoritics & Planetary Science;2021-12

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