Heat-flow data from southeastern Oregon [electronic resource]
Geothermal Legacy.
Saved in:
Online Access: |
Online Access |
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Corporate Authors: | , |
Format: | Government Document Electronic eBook |
Language: | English |
Published: |
Oak Ridge, Tenn. : Oak Ridge, Tenn. :
United States. Dept. of Energy. Technical Information Center ; distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy,
1976.
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Subjects: |
MARC
LEADER | 00000nam a22000003u 4500 | ||
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003 | CoU | ||
006 | m d f | ||
007 | cr ||||||||||| | ||
008 | 120401e19760101tnu ot f0|||||eng|d | ||
005 | 20230817214029.2 | ||
035 | |a (TOE)ost5665398 | ||
035 | |a (TOE)5665398 | ||
040 | |a TOE |c TOE | ||
049 | |a GDWR | ||
072 | 7 | |a 15 |2 edbsc | |
086 | 0 | |a E 1.99:usgs-ofr-76-217 | |
088 | |a usgs-ofr-76-217 | ||
245 | 0 | 0 | |a Heat-flow data from southeastern Oregon |h [electronic resource] |
260 | |a Oak Ridge, Tenn. : |b United States. Dept. of Energy. Technical Information Center ; |a Oak Ridge, Tenn. : |b distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy, |c 1976. | ||
300 | |a Pages: 55 : |b digital, PDF file. | ||
336 | |a text |b txt |2 rdacontent. | ||
337 | |a computer |b c |2 rdamedia. | ||
338 | |a online resource |b cr |2 rdacarrier. | ||
500 | |a Published through the Information Bridge: DOE Scientific and Technical Information. | ||
500 | |a 01/01/1976. | ||
500 | |a "usgs-ofr-76-217" | ||
500 | |a Sass, J.H.; Munroe, R.J.; Urban, T.C.; Galanis, S.P. Jr. | ||
520 | 3 | |a With the exception of values from two holes drilled within 2 km of Mickey Hot Springs, 17 new heat-flow values in southeastern Oregon are within or somewhat below the range one would normally expect in nonanomalous parts of the North American Cordillera. This is not surprising for a region in which most igneous rocks on the surface are 5 m.y. old or more. There is a suggestion of a thermal anomaly associated with the very young (late Pleistocene or Holocene) Diamond Craters lava field, and the thermal regime on both sides of Steens Mountain seems to be controlled, to some degree, by lateral and vertical movement of water. | |
520 | 0 | |a Geothermal Legacy. | |
650 | 7 | |a Temperature Distribution. |2 local. | |
650 | 7 | |a Volcanic Rocks. |2 local. | |
650 | 7 | |a Heat Flow. |2 local. | |
650 | 7 | |a Lava. |2 local. | |
650 | 7 | |a Rocks. |2 local. | |
650 | 7 | |a Boreholes. |2 local. | |
650 | 7 | |a Usa. |2 local. | |
650 | 7 | |a North America. |2 local. | |
650 | 7 | |a Cavities. |2 local. | |
650 | 7 | |a Pacific Northwest Region. |2 local. | |
650 | 7 | |a Oregon. |2 local. | |
650 | 7 | |a Igneous Rocks. |2 local. | |
650 | 7 | |a Thermal Springs. |2 local. | |
650 | 7 | |a Geothermal Energy. |2 edbsc. | |
710 | 2 | |a Geological Survey (U.S.). |4 res. | |
710 | 1 | |a United States. |b Department of Energy. |b Technical Information Center. |4 res. | |
710 | 1 | |a United States. |b Department of Energy. |b Office of Scientific and Technical Information. |4 dst. | |
856 | 4 | 0 | |u http://www.osti.gov/servlets/purl/5665398-gPuCjo/native/ |z Online Access |
907 | |a .b72111938 |b 03-07-23 |c 11-08-12 | ||
998 | |a web |b 11-08-12 |c f |d m |e p |f eng |g tnu |h 0 |i 1 | ||
956 | |a Information bridge | ||
999 | f | f | |i 15f354fb-9e4b-5dca-b4d2-ad94a329949c |s 39273afd-3b98-5540-a763-965368da0e59 |
952 | f | f | |p Can circulate |a University of Colorado Boulder |b Online |c Online |d Online |e E 1.99:usgs-ofr-76-217 |h Superintendent of Documents classification |i web |n 1 |