Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Elements Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Elements; January 2005; v. 1; no. 1; p. 39-43; DOI: 10.2113/gselements.1.1.39
© 2005 Mineralogical Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Zolensky, M. E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Extraterrestrial Water

Michael E. Zolensky1

1 Astromaterials Research and Exploration Science
NASA Johnson Space Center, Houston, TX 77058 USA
E-mail: michael.e.zolensky{at}nasa.gov

Abundant water ice was formed in the solar nebula outward of about 4 astronomical units and, during the entire history of the solar system, has been carried into the inner solar system in icy and hydrated bodies. We do not know which sources of water dominated in the inner solar system, but micrometeorites derived from C-class asteroids may have been most important. Today, hydrous materials occur throughout the solar system from Jupiter inwards, at least. Significant quantities of liquid water are, however, probably present only on Earth and some icy moons of Jupiter and possibly Saturn.

KEYWORDS: water, solar system, carbonaceous chondrites, asteroids, meteorites, comets, moons, planets, aqueous alteration







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of America