Porous, S-bearing silica in metal-sulfide nodules and in the interchondrule clastic matrix in two EH3 chondrites

Author:

Lehner S. W.1ORCID,Németh P.2,Petaev M. I.34,Buseck P. R.1

Affiliation:

1. School of Earth and Space Exploration; Arizona State University; Tempe Arizona 85287 USA

2. Institute of Materials and Environmental Chemistry; Research Center for Natural Sciences; Hungarian Academy of Sciences; Magyar Tudósok Körútja 2 H-1117 Budapest Hungary

3. Department of Earth and Planetary Sciences; Harvard University; Cambridge Massachusetts 02138 USA

4. Solar, Stellar, and Planetary Sciences; Harvard-Smithsonian CfA; Cambridge Massachusetts 02138 USA

Funder

National Aeronautics and Space Administration

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Reference38 articles.

1. Chemical bonding state of S in Na2S-SiO2 glasses;Asahi;Journal of the Ceramic Society of Japan,1998

2. Study of the phase separation in amorphous silicon oxycarbide glasses under heat treatment;Brequel;Nanostructured Materials,1999

3. Normal and reverse zoning in niningerite: A novel key parameter to the thermal histories of EH-chondrites;Ehlers;Geochimica et Cosmochimica Acta,1988

4. Fagan T. J. Kataoka S. Matsui K. Norose K. Yoshida A. 2008 Equilibration reactions between silicates, sulfides, and Fe,Ni metal in EH chondrites

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