Nature and degree of aqueous alteration in CM and CI carbonaceous chondrites-Reference-Cited by-同舟云学术

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Nature and degree of aqueous alteration in CM and CI carbonaceous chondrites

Published:2013-08 Issue: Volume: Page:n/a-n/a
ISSN:1086-9379
Container-title:Meteoritics & Planetary Science
language:en
Short-container-title:Meteorit Planet Sci

Author:

Takir Driss¹,Emery Joshua P.¹,Mcsween Harry Y.¹,Hibbitts Charles A.²,Clark Roger N.³,Pearson Neil³,Wang Alian⁴

Affiliation:

1. Department of Earth & Planetary Sciences and Planetary Geosciences Institute; University of Tennessee; Knoxville; Tennessee; 37996; USA

2. Johns Hopkins University Applied Physics Laboratory; Laurel; Maryland; 20273; USA

3. U.S. Geological Survey; Denver; Colorado; 80225; USA

4. Department of Earth and Planetary Sciences and McDonnell Center for Space Sciences; Washington University; St. Louis; Missouri; 63130; USA

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/maps.12171/fullpdf

Reference64 articles.

1. Hydrous mineralogy of CM and CI chondrites from infrared spectroscopy and their relationship with low albedo asteroids;Beck;Geochimica et Cosmochimica Acta,2010

2. Extraterrestrial organic compounds in meteorites;Botta;Survey of Geophysics,2002

3. Amino acids in Antarctic CM1 meteorites and their relationship to other carbonaceous chondrites;Botta;Meteoritics & Planetary Science,2007

4. Phyllosilicates in the matrix of the unique carbonaceous chondrite, LEW 85332 and possible implications for aqueous alteration of CI chondrites;Brearley;Meteoritics & Planetary Science,1997

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