Self-reversed magnetization held by martite in basalt flows from the 1.1-billion-year-old Keweenawan rift, Canada-Reference-Cited by-同舟云学术

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Self-reversed magnetization held by martite in basalt flows from the 1.1-billion-year-old Keweenawan rift, Canada

Published:2011-05 Issue:1-2 Volume:305 Page:171-184
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Swanson-Hysell Nicholas L.,Feinberg Joshua M.,Berquó Thelma S.,Maloof Adam C.

Publisher

Elsevier BV

Subject

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

Reference68 articles.

1. Cation diffusion in titanomagnetites;Aragon;Contrib. Mineralog. Petrol.,1984

2. Banerjee, S., 1963. Magnetic properties of rocks and minerals. Ph.D. thesis, University of Cambridge.

3. Crystallographic texture of the magnetite–hematite transformation: evidence for topotactic relationships in natural samples from Quadrilátero Ferrífero, Brazil;Barbosa;Am. Mineralog.,2010

4. Oriented transformations in iron oxides and hydroxides;Bernal;Nature,1957

5. Improving the validity of hyperfine field distributions from magnetic alloys, part I: unpolarized source;Brand;Nucl. Instrum. Meth. Phys. Res. B,1987

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