O2volumes at high pressure from KClO4decomposition: D″ as a siderophile element pump instead of a lid on the core-Reference-Cited by-同舟云学术

O2volumes at high pressure from KClO4decomposition: D″ as a siderophile element pump instead of a lid on the core

Author:

Walker D.¹,Clark S. M.²³,Cranswick L. M. D.¹²⁴,Johnson M. C.⁵,Jones R. L.²

Affiliation:

1. Lamont-Doherty Earth Observatory of Columbia University; Palisades New York 10964 USA

2. Daresbury Laboratory; CLRC; Warrington WA4 4AD UK

3. Advanced Light Source, LBNL; MS 80-101, 1 Cyclotron Road, Berkeley California 94720 USA

4. Department of Crystallography, Birkbeck College; University of London; Malet Street, Bloomsbury, London WCIE 7HX UK

5. Department of Geography and Environmental Engineering; United States Military Academy; West Point New York 10996 USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference57 articles.

4. Benedetti , L. R. Molecular systems at high pressures and temperatures: Solar system astronomy in a physics laboratory Berkeley 2001

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