Anhydrous partial melting of an iron-rich mantle II: primary melt compositions at 15 kbar-Reference-Cited by-同舟云学术

Anhydrous partial melting of an iron-rich mantle II: primary melt compositions at 15 kbar

Published:1994-01 Issue:3 Volume:115 Page:323-338
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Bertka Constance M.,Holloway John R.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00310771.pdf

Reference47 articles.

1. Baird AK, Clark BC (1981) On the original igneous source of Martian fines. Icarus 45:113?123

2. Bence AE, Albee AL (1968) Empirical correction factors for the electron microanalysis of silicates and oxides. J Geol 76:382?403

3. Bertka CM, Holloway JR (1988) Martian mantle primary melts: an experimental study of iron-rich garnet lherzolite minimum melt composition Proc Lunar Planet Sci Conf 18:723?739

4. Bertka CM, Holloway JR (1994a) Anhydrous partial melting of an iron-rich mantle I: subsolidus phase assemblages and partial melting phase relations at 10 to 30 kbar. Contrib Mineral Petrol 115:313?322

5. Bertka CM, Holloway JR (1994b) Pigeonite at solidus temperatures: implications for partial melting. (in press) J Geophys Res

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