Asteroidal Water Within Fluid Inclusion-Bearing Halite in an H5 Chondrite, Monahans (1998)-Reference-Cited by-同舟云学术

Asteroidal Water Within Fluid Inclusion-Bearing Halite in an H5 Chondrite, Monahans (1998)

Published:1999-08-27 Issue:5432 Volume:285 Page:1377-1379
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Zolensky Michael E.¹,Bodnar Robert J.²,Gibson Everett K.¹,Nyquist Laurence E.¹,Reese Young³,Shih Chi-Yu³,Wiesmann Henry³

Affiliation:

1. Mail Code SN2, NASA Johnson Space Center, Houston, TX 77058, USA.

2. Department of Geological Sciences, Virginia Tech, Blacksburg, VA 24061, USA.

3. Lockheed Martin Space Operations Company, Houston, TX 77058, USA.

Abstract

Crystals of halite and sylvite within the Monahans (1998) H5 chondrite contain aqueous fluid inclusions. The fluids are dominantly sodium chloride–potassium chloride brines, but they also contain divalent cations such as iron, magnesium, or calcium. Two possible origins for the brines are indigenous fluids flowing within the asteroid and exogenous fluids delivered into the asteroid surface from a salt-containing icy object.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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