Re-Os isotope systematics of Ni-Cu sulfide ores, Sudbury Igneous Complex, Ontario: evidence for a major crustal component-Reference-Cited by-同舟云学术

Re-Os isotope systematics of Ni-Cu sulfide ores, Sudbury Igneous Complex, Ontario: evidence for a major crustal component

Published:1991-08 Issue:4 Volume:105 Page:416-429
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Walker R.J.,Morgan J.W.,Naldrett A.J.,Li C.,Fassett J.D.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference44 articles.

1. Precise U-Pb zircon and baddeleyite ages for the Sudbury area;Krogh,1984

2. The main mass of the Sudbury Igneous Complex;Naldrett,1984

3. Gravity and magnetic characteristics of the Sudbury structure;Gupta,1984

4. B.T. Scribbins, D.R. Rae and A.J. Naldrett, Mafic and ultramafic inclusions in the Sublayer of the Sudbury Igneous Complex, Can. Mineral. 22, 67–75.

5. Sudbury structure Ontario: Some petrographic evidence for origin by meteorite impact;French;Science,1967

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