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. 1964 Dec;52(6):1433–1439. doi: 10.1073/pnas.52.6.1433
ICE VII, THE DENSEST FORM OF ICE*
Barclay Kamb
1,2, Briant L Davis
1,2
Barclay Kamb
1CALIFORNIA INSTITUTE OF TECHNOLOGY, PASADENA
2SOUTH DAKOTA SCHOOL OF MINES AND TECHNOLOGY, RAPID CITY
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Briant L Davis
1CALIFORNIA INSTITUTE OF TECHNOLOGY, PASADENA
2SOUTH DAKOTA SCHOOL OF MINES AND TECHNOLOGY, RAPID CITY
Find articles by Briant L Davis
1CALIFORNIA INSTITUTE OF TECHNOLOGY, PASADENA
2SOUTH DAKOTA SCHOOL OF MINES AND TECHNOLOGY, RAPID CITY
*
This paper is a joint contribution from the Division of the Geological Sciences, California Institute of Technology (no. 1301) and from the Institute of Geophysics and Planetary Physics, University of California, Los Angeles (no. 404). The experimental work was carried out at the latter institution, through the kind cooperation of George C. Kennedy and Leason H. Adams. The work was supported in part by grants from the National Science Foundation.
PMCID: PMC300465 PMID: 16591242
