Spontaneous movement of ions through calcite at standard temperature and pressure
Spontaneous movement of ions through calcite at standard temperature and pressure
About this item
Full title
Author / Creator
Publisher
London: Nature Publishing Group UK
Journal title
Language
English
Formats
Publication information
Publisher
London: Nature Publishing Group UK
Subjects
More information
Scope and Contents
Contents
At the resolution limits of traditional geochemical techniques, there is little evidence to challenge the common assumptions that, under the Earth's ambient surface conditions, dry calcite is static and that the bulk mineral behaves as a closed system. Solid-state diffusion has been recognized at elevated temperatures
1
,
2
,
3
,...
Alternative Titles
Full title
Spontaneous movement of ions through calcite at standard temperature and pressure
Authors, Artists and Contributors
Author / Creator
Identifiers
Primary Identifiers
Record Identifier
TN_cdi_proquest_miscellaneous_787344588
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_787344588
Other Identifiers
ISSN
0028-0836
E-ISSN
1476-4687
DOI
10.1038/24597
