Zobrazeno 1 - 10
of 35
pro vyhledávání: '"M.J. Aldrich"'
Publikováno v:
Journal of Volcanology and Geothermal Research. 45:59-69
The structural geology of the Platanares geothermal site in western Honduras, located about 25 km south of the northern boundary of the Caribbean plate, is the result of post Early Miocene extensional deformation. Normal faults, many with listric geo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f6b04a35a693b0dbecf3d0f9fd9446e2
https://doi.org/10.1016/0377-0273(91)90022-r
https://doi.org/10.1016/0377-0273(91)90022-r
Akademický článek
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Publikováno v:
Earth and Planetary Science Letters. 76:361-374
Fifty-one lamprophyre dikes of the Navajo volcanic field are randomly oriented in contrast to dikes of similar age from adjacent tectonic provinces. K Ar ages obtained on nine of these dikes indicate that they were emplaced between 28 and 19 m.y. ago
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d64f9a10979188e312400143f7bbeb74
https://doi.org/10.1016/0012-821x(86)90087-7
https://doi.org/10.1016/0012-821x(86)90087-7
Publikováno v:
Journal of Volcanology and Geothermal Research. 15:21-41
The Phase I prototype hot dry rock (HDR) geothermal system was developed in Precambrian basement rocks at Fenton Hill, New Mexico. Core and cuttings samples from the four deep wells indicate that the reservoir of this Phase I HDR system lies within a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::271f2820de5772b036e94fead5a24af1
https://doi.org/10.1016/0377-0273(83)90094-x
https://doi.org/10.1016/0377-0273(83)90094-x
Autor:
M.J. Aldrich, A.W. Laughlin
This map is one of a series of maps designed for hot dry rock geothermal assessment in Arizona, New Mexico, and the Trans-Peco area of the west Texas. The 3.0 m.y. cutoff age was selected because original heat has probably largely dissipated in older
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e987b8c60854b2ffeae7dbcbc6ead2b7
https://doi.org/10.2172/5171010
https://doi.org/10.2172/5171010
Autor:
M.J. Aldrich, A.W. Laughlin
As part of the assessment of the Hot Dry Rock geothermal energy potential of Arizona and New Mexico, a compilation of the locations and ages of volcanic rocks less than 5 Myr was made. The locations of those rocks less than 3 Myr are shown on a map o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::12daca41283196e7527a81639c508432
https://doi.org/10.2172/6376119
https://doi.org/10.2172/6376119
Review of the Electric Power Research Institute's (EPRI) method for calculating the geothermal resource base of a country shows that modifications are needed for several of the assumptions used in the calculation. These modifications include: (1) sep
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::650a51bed33e379754501f88834e7ddc
https://doi.org/10.2172/6376171
https://doi.org/10.2172/6376171
Petrologic, geochemical, and structural analyses of cores and cuttings obtained from 3000 to 4389-m true vertical depth in drill hole EE-2 indicate that this deeper part of the Precambrian section at Fenton Hill, New Mexico is composed primarily of a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::34c4ea1c914aa76e2e266729e780a8eb
https://doi.org/10.2172/6351947
https://doi.org/10.2172/6351947
The San Ignacio (La Tembladera) geothermal site is located on the north side of the Siria Valley, Departamento de Francisco Morazan, near the village of Barrosa. Hot springs are located along a northwest-trending fault scarp at the edge of the valley
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bcde2bd18c338a8af910faefd41e00f5
https://doi.org/10.2172/6147956
https://doi.org/10.2172/6147956
Autor:
M.J. Aldrich
Publikováno v:
Tectonophysics. 98:338-339
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d906bf4c384a5dea9adfae5543467d9b
https://doi.org/10.1016/0040-1951(83)90302-5
https://doi.org/10.1016/0040-1951(83)90302-5