Remanent magnetization in the contact zone between Columbia Plateau flows and feeder dikes: Evidence for groundwater layer at time of intrusion-Reference-Cited by-同舟云学术

Remanent magnetization in the contact zone between Columbia Plateau flows and feeder dikes: Evidence for groundwater layer at time of intrusion

Published:1980 Issue:B4 Volume:85 Page:1888
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Buchan K. L.,Schwarz E. J.,Symons D. T. A.,Stupavsky M.

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

Link

http://www.agu.org/journals/jb/v085/iB04/JB085iB04p01888/JB085iB04p01888.pdf

Reference35 articles.

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2. Chemical analyses of 305 basalt samples from the Columbia River Plateau, Washington, Oregon and Idaho, open file report;Brock,1973

3. Petrochemical stratigraphy and structure of the Columbia River basalt, Lewiston Basin area, Idaho-Washington;Camp,1976

4. Carslaw, H. S., , J. C., Jaeger, , Conduction of Heat in Solids, 2nd ed. Oxford University Press, New York, 1959,

5. Davis, S. N., , R. J. M., DeWiest, , Hydrogeology, John Wiley, New York, 1966,

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