Regional implications of heat flow of the Snake River Plain, Northwestern United States-Reference-Cited by-同舟云学术

Regional implications of heat flow of the Snake River Plain, Northwestern United States

Published:1989-08 Issue:2-4 Volume:164 Page:323-343
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Blackwell D.D.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference66 articles.

1. Quaternary and Neogene volcanic rocks, of the Snake River Plain, Idaho;Armstrong;Am. J. Sci.,1975

2. Evidence of former higher temperatures from alteration minerals, Bostic 1-A well, Mountain Home, Idaho;Arney;Geotherm. Resour. Counc. Trans.,1982

3. Evaluation of the hot dry rock geothermal potential of an area near Mountain Home, Idaho;Harding Lawson Associates;Los Alamos Natl. Lab. Rep. LA-9365-HDR,1982

4. Heat flow and energy loss in the western United States;Blackwell,1978

5. Heat flow in the northern Basin and Range Province;Blackwell,1983

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