Snowflake troctolite in the Hettasch intrusion, Labrador: Evidence for magma-mixing and supercooling in a plutonic environment-Reference-Cited by-同舟云学术

Snowflake troctolite in the Hettasch intrusion, Labrador: Evidence for magma-mixing and supercooling in a plutonic environment

Published:1980-06 Issue:4 Volume:72 Page:339-351
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Berg Jonathan H.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00371343.pdf

Reference55 articles.

1. Arndt, N.T.: Melting relations of ultramafic lavas (komatiites) at 1 atm and high pressure. Carnegie Inst. Washington, Yearb. 75, 555?562 (1976)

2. Arndt, N.T.: Partitioning of nickel between olivine and ultrabasic and basic komatiite liquids. Carnegie Inst. Washington, Yearb. 76, 553?557 (1977)

3. Arndt, N.T., Naldrett, A.J., Pyke, D.R.: Komatiitic and iron-rich tholeiitic lavas of Munro Township, northeast Ontario. J. Petrol. 18, 319?369 (1977)

4. Field Report 1973, Contr.;J.M. Barton Jr.,1974

5. Field Report 1972. Contr.;J.H. Berg,1973

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