3 edition of Geological investigation of the Socorro geothermal area found in the catalog.
Geological investigation of the Socorro geothermal area
Charles Edward Chapin
by New Mexico Energy Institute at New Mexico State University in [Las Cruces]
Written in English
|Statement||principal investigators, C. E. Chapin, A. R. Sanford, D. W. [i.e. L.] White ; R. M. Chamberlin, research assistant, G. R. Osburn, research assistant.|
|Contributions||Sanford, Allan R., 1927-, White, D. L. 1944-|
|LC Classifications||QE144.S6 C48|
|The Physical Object|
|Pagination||v, 70 p. :|
|Number of Pages||70|
|LC Control Number||79624742|
The New Mexico Geological Society field conference returns to the Socorro area after a lapse of 20 years (Guidebook 14). One of the advantages of returning to the site of a former field conference is the perspective gained on trends and progress in the geological sciences during the intervening years. Geochemical investigation of the Hohi geothermal area - Interpretation for analytical results of geothermal fluids out of test boreholes - Journal/Book_names=Report, Geological Survey of Japan! Research in the Hohi Geothermal Area. Publish_Country=Japan. number= pages= Publish_year= Publisher=Geological Survey of Japan.
The Upper Centennial Valley, Beaverhead and Madison Counties, Montana: An Investigation of Resources Utilizing Geological, Geophysical, Hydrochemical, and Geothermal Methods Montana Bureau of Mines and Geology, - Geology - 53 pages. Broadlands geothermal area geophysical survey. Rating Required Name Email Required incorporates the results of a number of geophysical methods which are now regarded as being well established for the investigation of new geothermal areas. The application of these results for the siting of investigatory deep drillholes has permitted these.
To purchase this publication in book format, please order GC ABSTRACT The Hueco Tanks geothermal area contains five known but now inactive hot wells (50° to 71°C). The area trends north-south along the east side of Tularosa-Hueco Bolson astride the Texas-New Mexico border approximately 40 km northeast of El : $5. Jornada del Muerto Wilderness Study Area, Socorro and Sierra Counties, New Mexico By Donald H. Richter and Richard W. Saltus U.S. Geological Survey George S. Ryan U.S. Bureau of Mines SUMMARY The Jornada del Muerto Wilderness Study Area (NM) inclu acres in Socorro and Sierra Counties in west-central New : Donald H. Richter, R.W. Saltus, George S. Ryan.
Elseviers dictionary of soil science
Relationship between trends in technological changes and patterns in vocational in-service education
The 2002 official patients sourcebook on yersiniosis
Clinical Supervision and Mentorship in Nursing
How to find the perfect job
Department of Correction furlough program.
Revised statutes of the State of Missouri, 1978
Four Greek poets
approach to Vedanta.
Understanding Signals and Systems
The impact of 7 July 2005 London Bomb attacks on Muslim communities in the EU
history of Vaughan Township
Human Desire and Economic Satisfaction
Geological investigation of the Socorro geothermal area. Final Report [C.E Chapin] on *FREE* shipping on qualifying offers.
The results of a comprehensive geological and geochemical study of the Socorro geothermal area are presented. The following are discussed: geologic setting, structural controls, stratigraphic controls, an ancient geothermal system, modern magma bodies, geothermal potential of the Socorro area, and the Socorro transverse shear zone.
(MHR). Geological investigation of the Socorro geothermal area: final report: Publication Type: Book: Place Published: Las Cruces, NM: Publisher: New Mexico Energy Institute at New Mexico State University: Year: Keywords: Geology – New Mexico – Socorro Region, Geothermal resources – New Mexico – Socorro Region: Call Number: GB N6 G URL.
Get this from a library. Geologic and geophysical investigation of the Beowave geothermal area, north-central Nevada.
[Mary Lou C Zoback;]. Summary. Geothermal energy stands out because it can be used as a baseload resource. This book, unlike others, examines the geology related to geothermal applications.
Geology dictates (a) how geothermal resources can be found, (b) the nature of the geothermal resource (such as liquid- or vapor-dominated) and. PDF | Investigation of Seferihisar-Balcova geothermal area by environmental isotopes.
| Find, read and cite all the research you need on ResearchGate. Pilgrim Hot Springs, located on the Seward Peninsula in west-central Alaska, is characterized by hot springs, surrounding thawed regions, and elevated lake temperatures.
The area is of interest because of its potential for providing renewable energy for Nome and nearby rural communities. We performed ground and airborne geophysical investigations of the Pilgrim Springs geothermal area Author: Jonathan M.G.
Glen, Darcy K. McPhee, Paul A. Bedrosian. low-temperature geothermal exploration methods in Socorro, New Mexico. The Socorro Geothermal Area in New Mexico represents a low-temperature, geothermal system demonstrated by several hot springs and an exploration slim hole drilled at the base of Socorro Peak.
Low temperature reservoirs typically lack surface manifestations and equilibrated. Groundwater will circulate in a permeable medium by a process of natural convection if a sufficient temperature gradient exists. In the vicinity of th Cited by: Spiegel () described the hydrology of a square-mile area in the northeast part of the county.
A detailed hydrologic study of the southeastern part of the county was done by Weir (). Summers () presented information on the geothermal area 3 miles west of by: 5. Geothermal assessment of part of the east shore area, Davis and Weber Counties, Utah (Report of investigation / Utah Geological and Mineral Survey) [Robert H Klauk] on *FREE* shipping on qualifying offers.
The following are discussed: geologic setting, structural controls, stratigraphic controls, an ancient geothermal system, modern magma bodies, geothermal potential of the Socorro area Author: Kimberly Elkins. Get this from a library. Geologic and Geophysical Investigation of the Beowawe Geothermal Area, North-Central Nevada.
[M L C Zoback; Stanford University. School of Earth Sciences.]. Research in the Hohi geothermal Area. and a great selection of related books, art and collectibles available now at - AbeBooks Passion for books. Audio Books & Poetry Community Audio Computers & Technology Music, Arts & Culture News & Public Affairs Non-English Audio Spirituality & Religion.
Librivox Free Audiobook. Podcasts. Featured software All software latest This Just In Old School Emulation MS-DOS Games Historical Software Classic PC Games Software Library.
pages, maps and diagrams. Contributions are in Japanese with resumees in English. Report No. Geological Survey of Japan. Kimbara Keiji, Hase Hirokazu and Ogawa Katsuro (Ed.).
Historical background of geothermal research in the Sengan area. Kimbara Keiji and Hase Hirokazu; Summary of the researches in the Sengan geothermal area, Northeast Japan. Preliminary investigation of the source of lead and strontium in deep geothermal brines underlying the Salton Sea geothermal areaCited by: New Mexico Bureau of Geology & Mineral Resources New Mexico Institute of Mining & Technology Leroy Place Socorro, NM pages, maps and diagrams.
Contributions are in Japanese. Report No. Geological Survey of Japan. Historical background of geothermal research in the Geological Survey: Yamada Keiichi; Research in the Hohi geothermal area: Outline and summary: Hase Hirokazu, Ogawa Katsuro and Kimbara Keiji; Volcanic activity in relation to the geologic structure in the.
Since the s, the USGS and its partners, the State Geological Surveys, have been producing high quality, standardized geologic maps of the Nation. Check out the National Geologic Map Database (NGMDB), which is the National archive of these maps and related geoscience reports.
SPARROW model results of long-term mean-annual total nitrogen and. along with geological, geophysical, and hydrological methods, to define a potential buried geothermal system in Socorro, New Mexico.
Geophysical studies, along with projection of mapped geology suggest that a buried geothermal reservoir may occur approximately feet below the surface. Soil geochemical patterns at the surface indicate the.The Cameroon Volcanic Line (CVL) belongs to the African plate and extends over km distance from the volcanic islands of the Gulf of Guinea to the Lake Chad (Fig.
1A and B).It is situated at the northern edge of Congo craton and consists of plutonic complexes and volcanos following a general alignment N30° (Marcel et al., a).The recent volcanic activities of the Author: Kasi Njeudjang, Jean Marcel Abate Essi, Janvier Domra Kana, William Assatse Teikeu, Philippe Njandjo.Citation: Gross, Gerado W.; Wilcox, Ralph,Groundwater circulation in the Socorro geothermal area, in: Socorro region II, Chapin, C.
E., New Mexico Geological.