A closer look at remanence-dominated aeromagnetic anomalies: Rock magnetic properties and magnetic mineralogy of the Russell Belt microcline-sillimanite gneiss, northwest Adirondack Mountains, New York

Author:

McEnroe Suzanne A.,Brown Laurie L.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference71 articles.

1. Balsley , J. R. Total aeromagnetic intensity and geologic map of the Stark, Childwold and part of Russell quadrangles 1954

2. Correlation of reversed remanent magnetism and negative anomalies with certain minerals;Balsley;J. Geomagn. Geoelectr.,1954

3. Remanent magnetism of the Russell Belt of gneisses, northwest Adirondack Mountains, New York;Balsley;Adv. in Phys.,1957

4. Iron titanium oxide minerals, rocks, and aeromagnetic anomalies of the Adirondack area, New York;Balsley;Econ. Geol.,1958

5. New grain size limits for paleomagnetic stability in hematite;Banerjee;Nature Phys. Sci.,1971

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