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Статті в журналах з теми "Geothermal geology"
TOMASZEWSKA, Barbara, Marta DENDYS, and Leszek PAJĄK. "ANALYSIS OF HYDROGEOLOGICAL CONDITIONS SUPPORTED BY A MATHEMATICAL MODELING AS THE BASIC STAGE OF INVESTMENT PROJECTS IN GEOTHERMY FIELD." Biuletyn Państwowego Instytutu Geologicznego 471 (October 1, 2018): 179–84. http://dx.doi.org/10.5604/01.3001.0012.4931.
Повний текст джерелаMazzoli, Stefano. "Geothermal Energy and Structural Geology." Energies 15, no. 21 (October 31, 2022): 8074. http://dx.doi.org/10.3390/en15218074.
Повний текст джерелаDai, Peng, Kongyou Wu, Gang Wang, Shengdong Wang, Yuntao Song, Zhenhai Zhang, Yuehan Shang, Sicong Zheng, Yinsheng Meng, and Yimin She. "Geothermal Geological Characteristics and Genetic Model of the Shunping Area along Eastern Taihang Mountain." Minerals 12, no. 8 (July 22, 2022): 919. http://dx.doi.org/10.3390/min12080919.
Повний текст джерелаZhang, Xiao Ling, Hong Zhan Liu, and Kang Chen. "Geothermal Geology Characteristic and Origin Analysis of Shilin Basin in Yunnan Province." Advanced Materials Research 779-780 (September 2013): 1449–52. http://dx.doi.org/10.4028/www.scientific.net/amr.779-780.1449.
Повний текст джерелаShang, Yun Hu, Li Qing Liang, Peng Yuan Xu, An Da Zhang, and Yang Shen. "Prospecting and Evaluation of Geothermal Resources in Julang Pasture Area, Lindian County." Applied Mechanics and Materials 501-504 (January 2014): 451–54. http://dx.doi.org/10.4028/www.scientific.net/amm.501-504.451.
Повний текст джерелаOgoso-Odongo, Meshack E. "Geology of the Olkaria geothermal field." Geothermics 15, no. 5-6 (January 1986): 741–48. http://dx.doi.org/10.1016/0375-6505(86)90087-8.
Повний текст джерелаWood, C. P. "Geology of the rotorua geothermal system." Geothermics 21, no. 1-2 (February 1992): 25–41. http://dx.doi.org/10.1016/0375-6505(92)90066-i.
Повний текст джерелаSONG, Guofeng, Xianzhi SONG, Gensheng LI, Ruina XU, Wenjiong CAO, and Chenru Zhao. "Multi‐objective Optimization of Geothermal Extraction from the Enhanced Geothermal System in Qiabuqia Geothermal Field, Gonghe Basin." Acta Geologica Sinica - English Edition 95, no. 6 (December 2021): 1844–56. http://dx.doi.org/10.1111/1755-6724.14875.
Повний текст джерелаYan, Hua, Zhi Yuan Ma, Ting Li, and Guang Liang Niu. "Environmental Isotope Hydrogeochemical Characteristics and Instructions of Geothermal Water in Xianyang Urban Area." Advanced Materials Research 518-523 (May 2012): 4161–64. http://dx.doi.org/10.4028/www.scientific.net/amr.518-523.4161.
Повний текст джерелаCheng, Arthur. "President's Page: Geothermal energy: Current and future." Leading Edge 41, no. 9 (September 2022): 588–89. http://dx.doi.org/10.1190/tle41090588.1.
Повний текст джерелаДисертації з теми "Geothermal geology"
Malkemus, Donnel Alexander. "Geothermometry of Two Cascade Geothermal Systems." PDXScholar, 2016. https://pdxscholar.library.pdx.edu/open_access_etds/3369.
Повний текст джерелаSavage, Shannon Lea. "Mapping changes in Yellowstone's geothermal areas." Thesis, Montana State University, 2009. http://etd.lib.montana.edu/etd/2009/savage/SavageS0809.pdf.
Повний текст джерелаSpake, Phillip. "Geothermal Exploration North of Mount St. Helens." Master's thesis, Temple University Libraries, 2019. http://cdm16002.contentdm.oclc.org/cdm/ref/collection/p245801coll10/id/585881.
Повний текст джерелаM.S.
Active seismicity and volcanism north of Washington state’s Mount St. Helens provide key ingredients for hydrothermal circulation at depth. This broad zone of seismicity defines the St. Helens Seismic Zone, which extends well north of the volcanic edifice below where several faults and associated fractures in outcrop record repeated slip, dilation, and alteration indicative of localized fluid flow. Candidate reservoir rocks for a geothermal system include marine metasediments overlain by extrusive volcanics. The colocation of elements comprising a geothermal system at this location is tested here by analysis of the structures potentially hosting a reservoir, their relationship to the modern stress state, and temperature logs to a depth of 250 m. Outcrop mapping and borehole image log analysis down to 244 m document highly fractured volcaniclastic deposits and basalt flows. Intervening ash layers truncate the vertical extent of most structures. However, large strike slip faults with well-developed fault cores and associated high fracture density cross ash layers; vein filling and alternation of the adjacent host rock in these faults suggest they act as vertically extensive flow paths. These faults and associated fractures record repeated slip, dilation, and healing by various dolomite, quartz, and hematite, as well as clay alteration, indicative of long-lived, localized fluid flow. In addition, where these rocks are altered by igneous intrusion, they host high fracture density that facilitated heat transfer evidenced by associated hydrothermal alteration. Breakouts in image logs indicate the azimuth of SHmax in the shear zone is broadly consistent with both the GPS plate convergence velocity field as well as seismically active strike slip faults and strike-slip faults mapped in outcrop and borehole image logs. However, the local orientation of SHmax varies by position relative to the edifice and in some cases with depth along the borehole making a simple regional average SHmax azimuth misleading. Boreholes within the seismic zone display a wider variety of fracture attitudes than those outside the shear zone, potentially promoting permeability. Temperature profiles in these wells all indicate isothermal conditions at average groundwater temperatures, consistent with rapidly flowing water localized within fractures. Together, these results indicate that the area north of Mount Saint Helens generates and maintains porosity and permeability suggesting that conditions necessary for a geothermal system are present, although as yet no modern heat source or hydrothermal circulation was detected at shallow depth.
Temple University--Theses
Varriale, Jerome A. "The MH-2 Core from Project Hotspot: Description, Geologic Interpretation, and Significance to Geothermal Exploration in the Western Snake River Plain, Idaho." DigitalCommons@USU, 2016. https://digitalcommons.usu.edu/etd/4677.
Повний текст джерелаMiller, Joshua K. "A conceptual model of the Pilgrim Hot Springs geothermal system, Seward Peninsula, Alaska." Thesis, University of Alaska Fairbanks, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1550238.
Повний текст джерелаThis work has developed a conceptual geological model for the Pilgrim Hot Springs geothermal system supporting the exploration, assessment and potential development of this resource for direct use and electric power production. The development of this model involved the analysis of a variety of subsurface and geophysical data and the construction of a 3D lithostratigraphic block model. Interpretation of the data and block model aimed to establish the most likely scenario for subsurface geothermal fluid flow. As part of this work, well cuttings were analyzed for permeability and correlated with geophysical logs from well to well to constrain the stratigraphic architecture of the unconsolidated sediments. Hydrothermal alteration of the sediments and bedrock core was also studied through reflectance spectroscopy and methylene blue titration in order to investigate past fluid migration pathways. The structure of the basin was interpreted through geophysical surveys including aeromagnetic resistivity, isostatic gravity, and magnetotelluric resistivity. Based on temperature, well logs, geophysical surveys, and lithologic data, the system is subdivided into a shallow outflow aquifer and a deeper reservoir beneath a clay cap connected by a conduit with 91°C hydrothermal fluid upflow. Stratigraphic correlations indicate several clay layers throughout the section with a dominant clay cap at 200-275 m depth. Extensive pyritization and the clay mineral assemblage suggest an argillic-style alteration facies indicative of past temperatures at or slightly elevated above current conditions of hydrothermal activity at Pilgrim Hot Springs. The conceptual model supports production from this resource in those subsurface zones where there is sufficient permeability and connectivity with the upflow zone.
Faizy, Shelly Mardhia. "Assessing a Modeling Standard in Volcanic-Geothermal Systems: the Effects of the Lower System Boundary." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-438664.
Повний текст джерелаMcLachlan, Holly S. "Stratigraphy, Structure, and Fluid Flow at the Soda Lake Geothermal Field, Western Nevada, USA." Thesis, University of Nevada, Reno, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10841261.
Повний текст джерелаThis study assessed the geologic setting of the Soda Lake geothermal field, which lies in the southern part of the Carson Sink basin of northwestern Nevada within the Basin and Range of the western USA. The Basin and Range is a world-class geothermal province with significant untapped potential, particularly in blind (no surface hot springs or steam vents) geothermal systems. Blind systems probably comprise the majority of geothermal resources in the region, with many lying buried under thick accumulations of sediments in the broad basins that make up >50% of the province. Locating fault-hosted blind geothermal systems in these basins is challenging, and identifying the most prospective parts of these systems is even more demanding. The Soda Lake geothermal field is one of the more deeply buried known systems in this region. This study was undertaken to elucidate the stratigraphic and structural framework of the Soda Lake field, and to determine the probable controls on fluid flow in the production areas. Due to the depth of basin-fill sediments at the Soda Lake field, the structural setting and specific controls on fluid flow are not discernable at the surface. However, the Soda Lake geothermal field has produced electricity for over 30 years, and a wealth of subsurface data has been acquired since the field was first targeted for geothermal exploration in 1972-73. The abundant well data and geophysical surveys in particular provided a foundation for investigation of the geologic setting of the field.
This study was divided into three major parts. In the initial part of the study, a stratigraphic framework was developed for the Soda Lake area from analysis of cuttings, borehole geophysical logs, and radiometric dates of key igneous units. It was validated against exposed stratigraphic sections in the surrounding ranges and interpreted basin-fill sections derived from wells across the Carson Sink basin. Pursuant to this in the second part of the study, a comprehensive 3D geologic model of the Soda Lake field was construct from three inputs: 1) the new stratigraphic framework model, 2) bedding attitude estimates from seismic reflection surveys and borehole logs, and 3) a fault framework derived from both well data and geophysical surveys. The Soda Lake fault framework had been modeled from seismic reflection and borehole data in previous studies. In this study, one of the seismic fault pick sets was enhanced along strike and extended to >2 km depth using well data and forward modeled gravity. This enhanced fault framework served as the initial input to the Soda Lake geologic model. A ‘horizon model’ based on stratigraphic well intercepts and attitude data was then built around the fault framework to generate a 3D geologic block model for the Soda Lake field. In the final phase of this study, the Soda Lake temperature anomaly was modeled in a series of cross-sections extracted from the geologic model. The temperature anomaly was interpreted in context with the geologic model and production data in order to identify the main upwelling and outflow conduits. Key controls on fluid upwelling and probable fluid flow pathways were catalogued based on the spatial relationship between the temperature anomaly and the geologic model of the field area.
There are three major stratigraphic divisions at the Soda Lake geothermal field. The field is situated in and beneath ∼900-1100 m of unconsolidated basin-fill sediments. The basin-fill section is divided into an upper 300-500 m thick, relatively coarse-grained, quartzo-feldspathic unit, and a lower ∼150-300 m thick mud-rich unit. The unconsolidated basin fill is interrupted by a 5.1 Ma trachyandesite body that is up to ∼750 m thick in the central part of the Soda Lake well field. The body consists of a buried vent edifice near one of the main production wells, 50-90 m thick outflow aprons, and a conical root on the west side of the well field that can be traced to the Miocene bedrock contact. About 1 km of Miocene bedrock underlies the basin-fill section. The Miocene bedrock section is dominated by mafic lavas, interbedded with lesser tuff, clastic sedimentary rocks, and minor limestone. No early Miocene or Oligocene strata have been found at the Soda Lake field area. The middle to late Miocene section overlies Triassic-Jurassic metamorphic basement and Jurassic-Cretaceous granite. (Abstract shortened by ProQuest.)
Kent, Tyler. "Comparing Deformation at Soda Lake Geothermal Field from GPS and 3D Seismic." Thesis, University of Nevada, Reno, 2013. http://pqdtopen.proquest.com/#viewpdf?dispub=1540191.
Повний текст джерелаThe transition between the two distinct structural regimes of the Walker Lane and the Basin and Range allows for complex transtensional fault interactions. The Carson Sink is the surface expression of the interaction of shear and extensional strains that cause both crustal extension and block rotation. This study investigates this tectonic shift at the Soda Lake geothermal field by comparing the direction and rate of deformation from both regional GPS and a 34 sq km 3D seismic survey. The GPS stations in the region estimate the strain field by comparing tensor solutions that show changing direction and magnitude of strain across the Carson Sink. Using stations surrounding the Soda Lake 3D seismic survey, the strain tensor produced is comparable in orientation to Basin and Range strain but has larger magnitudes. To quantify deformation within the Soda Lake 3D seismic survey, we calculate fault dip and offset of a deformed paleo-planer lacustrine mudstone. Plotting the mean dip direction of the faults in the seismic reflectivity, matches the mean surrounding GPS extensional direction, suggesting fault displacement is likely to be normal dipslip. Using a minimum age of 0.51 Ma from nearby sedimentation rates, the measured extension across the 5.4 km length of this study has a rate of 0.19 mm/yr. This is quite a high value for Basin and Range extension and it is likely a result of some influence from the Northern Walker Lane. The lack of an obvious piercing point for shear observed within the seismic volume precludes a clear estimate of strike-slip related motion within the Soda Lake 3D seismic survey. Clear extension and a large fault bend, indicates a localized relay ramp model. With focused extension indicated by two late Quaternary extrusive volcanic bodies, a model of a transtensional pull-apart basin is also considered. Given the few mapped intrabasinal faults at the surface, this study gives a unique view into fault offsets inside the Carson Sink.
Gestsson, Einar Bessi. "Geothermal Potential of Sub-Volcanic Intrusions in a Typical Caldera Setting." Thesis, Uppsala universitet, Mineralogi, petrologi och tektonik, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-354072.
Повний текст джерелаVulkaner är en viktig energikälla i många länder runt om i världen. Geotermisk vätska och ånga av högtemperatur som finns i vulkanområden kan utnyttjas för bland annat elproduktion och fjärrvärme. Värmekällan till de geotermiska områdena är magma som ligger ytligt i jordskorpan. All magma når inte ytan i utbrott, utan stannar under vulkanen i form av magmaintrusioner. Intrusionerna av olika former och storlekar utgör ett nätverk som tillsammans utgör vulkanens magma transportsystem. I denna studie studeras en uppsättning av magmaintrusioner på nordöstra Island. Intrusionerna har en gång befunnit sig längre ner i jordskorpan under ett aktivt vulkanområde men exponeras nu vid ytan på grund av glacial erosion. Intrusionernas storlek och form varierar, men de flesta återfinns som gångar, både vertikala och horisontella. När en magmatintrusion bildas värms omkringliggande berggrund och grundvatten upp. Studiens fokus är att undersöka hur temperaturfördelningen i omgivningen skiljer sig vid en stor intrusion jämfört med flera mindre intrusioner med totalt samma volym. Även effekten från olika typer av berggrund runt intrusionerna studerades genom att jämföra temperaturfördelningen och kylningstiderna för intrusioner i tre vanliga bergarter. Numerisk modellering användades för att besvara dessa frågor. Bergarternas fysiska och termiska egenskaper krävdes som ingångsparametrar för den numeriska modelleringen. Parametrana uppskattades genom laboratorieexperiment och termometriberäkningar från fältprover. Värden från publicerat material användes också i modelleringen. Resultaten från den numeriska modelleringen antyder att högre maximivärden för temperaturen nås i berget över en stor, enskild intrusion jämfört med flera mindre intrusioner. När man jämför vertikala og horisontella gångar, ökar de vertikala gångarna berggrundens temperatur mer än de horisontella, medan medeltemperaturen ökar mer över horisontella gångar än i vertikala gångar. Trots den numeriska modellens förenklade struktur är förhoppningen att den nya datan kan inspirera vidare forskning, och bidra till en bättre förståelse om förhållandet mellan grunda magmaintrusioner och geotermiska system.
Skog, Gabriella. "Current Status and Future Outlook of Geothermal Reinjection: A Review of the Ongoing Debate." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-383963.
Повний текст джерелаКниги з теми "Geothermal geology"
Yang, Jianwen. Geothermal energy: Technology, and geology. Hauppauge, N.Y: Nova Science Publishers, 2012.
Знайти повний текст джерелаGeothermal energy in the USSR: A survey of resources, methodology, geology, and use. Falls Church, VA (7700 Leesburg Pike, #212, Falls Church 22043): Delphic Associates, 1985.
Знайти повний текст джерелаGürler, Barbaros. Die Geologie der Umgebung von Basel mit Hinweisen über die Nutzungsmöglichkeiten der Erdwärme. Bern: Stämpfli ₊ Cie, 1987.
Знайти повний текст джерелаLeiss, Bernd. Neue Untersuchungen zur Geologie der Leinetalgrabenstruktur: Bausteine zur Erkundung des geothermischen Potentials der Region Göttingen. Göttingen: Universitätsverlag Göttingen, 2011.
Знайти повний текст джерелаMyron, Dorfman, Morton Robert A, University of Texas at Austin. Center for Energy Studies., University of Texas at Austin. Bureau of Economic Geology., and University of Texas at Austin. College of Engineering., eds. Geopressured-geothermal energy: Proceedings of the Sixth U.S. Gulf Coast Geopressured-Geothermal Energy Conference : February 4-6, 1985, the University of Texas at Austin. New York: Pergamon Press, 1985.
Знайти повний текст джерелаBryan, T. Scott. Geysers: What they are and how they work. Niwot, Colo: Roberts Rinehart, 1990.
Знайти повний текст джерелаAllis, R. G. Subsidence prediction in New Zealand geothermal fields. Lower Hutt, N.Z: Institute of Geological & Nuclear Sciences Limited, 1998.
Знайти повний текст джерелаAnderson, John Edward. A preliminary geologic reconnaissance of the geothermal occurrences of the Wood River drainage area. Boise, Idaho: Idaho Dept. of Water Resources, 1985.
Знайти повний текст джерелаFriedman, Irving. Monitoring of thermal activity in southwest Yellowstone National Park. [Denver, CO]: U.S. Dept. of the Interior, Geological Survey, 1988.
Знайти повний текст джерелаWada, Nobuhiko. Nishi Iburi chiiki no chishitsu to jinetsu shigen. Sapporo-shi: Hokkaidōritsu Chika Shigen Chōsajo, 1988.
Знайти повний текст джерелаЧастини книг з теми "Geothermal geology"
Glassley, William E. "Geothermal Energy geothermal energy , Geology geothermal energy geology and Hydrology geothermal energy hydrology of." In Encyclopedia of Sustainability Science and Technology, 4179–90. New York, NY: Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4419-0851-3_230.
Повний текст джерелаGlassley, William E. "Geothermal Energy geothermal energy , Geology geothermal energy geology and Hydrology geothermal energy hydrology of." In Renewable Energy Systems, 761–71. New York, NY: Springer New York, 2013. http://dx.doi.org/10.1007/978-1-4614-5820-3_230.
Повний текст джерелаGlassley, William E. "Geology and Hydrology of Geothermal Energy." In Power Stations Using Locally Available Energy Sources, 23–34. New York, NY: Springer New York, 2018. http://dx.doi.org/10.1007/978-1-4939-7510-5_230.
Повний текст джерелаGlassley, William E. "Geothermal Energy, Geology and Hydrology of." In Encyclopedia of Sustainability Science and Technology, 1–13. New York, NY: Springer New York, 2017. http://dx.doi.org/10.1007/978-1-4939-2493-6_230-3.
Повний текст джерелаMahala, Subash Chandra. "Characteristics of Geothermal Gases." In Geology, Chemistry and Genesis of Thermal Springs of Odisha, India, 75–82. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-90002-5_6.
Повний текст джерелаMahala, Subash Chandra. "Uses of Geothermal Energy." In Geology, Chemistry and Genesis of Thermal Springs of Odisha, India, 91–100. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-90002-5_8.
Повний текст джерелаQiang, Wei, Y. Suzuki, N. Kawakami, S. Takasugi, and K. Kodama. "Three-Dimensional Simulation of Geologic Structures in Yakumo Geothermal Field, Southwest Hokkaido, Japan." In Mathematical Geology and Geoinformatics, 93–102. London: CRC Press, 2021. http://dx.doi.org/10.1201/9780429070891-10.
Повний текст джерелаNehler, Mathias, Philipp Mielke, Greg Bignall, and Ingo Sass. "New Methods of Determining Rock Properties for Geothermal Reservoir Characterization." In Engineering Geology for Society and Territory - Volume 6, 37–40. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09060-3_6.
Повний текст джерелаSuparman, Murni Sulastri, and Suci Sarah Andriany. "Wells Declivity Temperature Geothermal Field Bora-Sigi, Central Sulawesi, Indonesia." In Engineering Geology for Society and Territory - Volume 1, 373–78. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09300-0_71.
Повний текст джерелаVeld, H., W. J. J. Fermont, H. Kerp, and H. Visscher. "Geothermal history of the Carboniferous in South Limburg, the Netherlands." In Geology of Gas and Oil under the Netherlands, 31–43. Dordrecht: Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-0121-6_5.
Повний текст джерелаТези доповідей конференцій з теми "Geothermal geology"
Bondabou, K. "Advanced Mud Logging application to Shallow Geothermal." In Fourth EAGE Borehole Geology Workshop. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.2021626026.
Повний текст джерелаLipaev, Aleksander. "GEOTHERMAL RESERVOIR SIMULATION." In 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b13/s3.038.
Повний текст джерелаSumotarto, U., F. Hendrasto, M. Meirawati, and I. Azzam. "Geology of Arjosari geothermal area, Pacitan, East Java." In 2ND INTERNATIONAL CONFERENCE ON EARTH SCIENCE, MINERAL, AND ENERGY. AIP Publishing, 2020. http://dx.doi.org/10.1063/5.0007201.
Повний текст джерелаSilva Fragoso, Argelia, Luca Ferrari, and Gianluca Norini. "GEOLOGY OF THE DOMUYO GEOTHERMAL AREA, PATAGONIA, ARGENTINA." In 113th Annual GSA Cordilleran Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017cd-292791.
Повний текст джерелаWolpert, P., and T. Aigner. "Borehole Image Logs applied to Sequence Stratigraphy and Geothermal Exploration in Carbonates: an Integrated Workflow(UpperJurassic/Molasse basin)." In Third EAGE Borehole Geology Workshop. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201903301.
Повний текст джерелаGaffar, E., H. Permana, Y. Sudrajat, S. Indarto, H. Bakti, and H. Nurohman. "Geology , Geochemistry and Geophysics of Guci Geothermal Prospect Area, Central Java." In EAGE-HAGI 1st Asia Pacific Meeting on Near Surface Geoscience and Engineering. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800403.
Повний текст джерелаHassan, Syeda, and R. Shane McGary. "ASSESSING THE VIABILITY OF VIRGINIA GEOLOGY FOR GEOTHERMAL POWER PRODUCTION USING MAGNETOTELLURICS." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-345027.
Повний текст джерелаChitea, Florina. "GEOELECTRICAL METHODS APPLIED FOR PROSPECTING AN AREA WITH GEOTHERMAL POTENTIAL." In 14th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2014. http://dx.doi.org/10.5593/sgem2014/b11/s5.061.
Повний текст джерелаAlMuhaideb, Abdullah, and Sam Noynaert. "A 20 Years Systemic Study of Drilling Practices in a Geothermal Venture Reveals Insightful Findings." In SPE Annual Technical Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/206092-ms.
Повний текст джерелаRogan, Sasa. "PERSPECTIVES OF GEOTHERMAL ENERGY IN VOJVODINA WITH THE DEVELOPMENT OF TOURISM." In 13th SGEM GeoConference on SCIENCE AND TECHNOLOGIES IN GEOLOGY, EXPLORATION AND MINING. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/ba1.v1/s01.024.
Повний текст джерелаЗвіти організацій з теми "Geothermal geology"
Jessop, A. M. Geothermal energy [Chapter 6: Economic Geology]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/192373.
Повний текст джерелаUpdike, R. G. Engineering geology, technical feasibility study, Makushin geothermal power project, Unalaska, Alaska. Alaska Division of Geological & Geophysical Surveys, 1986. http://dx.doi.org/10.14509/1238.
Повний текст джерелаBlackett, R. E., M. A. Shubat, C. E. Bishop, D. S. Chapman, C. B. Forster, and C. M. Schlinger. The Newcastle geothermal system, Iron County, Utah: Geology, hydrology, and conceptual model. Office of Scientific and Technical Information (OSTI), March 1990. http://dx.doi.org/10.2172/7014844.
Повний текст джерелаLevey, Schon S. Subsurface Geology of the Fenton Hill Hot Dry Rock Geothermal Energy Site. Office of Scientific and Technical Information (OSTI), December 2010. http://dx.doi.org/10.2172/1012910.
Повний текст джерелаWitcher, J. C., W. R. Hahman, and C. A. Swanberg. Alpine 1/Federal: Temperature gradients, geothermal potential, and geology. Final report, Part 2. Office of Scientific and Technical Information (OSTI), June 1994. http://dx.doi.org/10.2172/10178176.
Повний текст джерелаNye, C. J., R. J. Motyka, D. L. Turner, and S. A. Liss. Geology and geochemistry of the Geyser Bight Geothermal area, Umnak Island, Aleutian Islands, Alaska. Alaska Division of Geological & Geophysical Surveys, 1992. http://dx.doi.org/10.14509/2480.
Повний текст джерелаHeiken, G., D. Eppler, K. Wohletz, W. Flores, N. Ramos, and A. Ritchie. Geology of the platanares geothermal site, Departamento de Copan, Honduras, Central America. Field report. Office of Scientific and Technical Information (OSTI), May 1986. http://dx.doi.org/10.2172/5509289.
Повний текст джерелаEppler, D. B., G. Heiken, K. Wohletz, W. Flores, J. R. Paredes, and W. A. Duffield. Geology of the Pavana geothermal area, Departamento de Choluteca, Honduras, Central America: Field report. Office of Scientific and Technical Information (OSTI), September 1987. http://dx.doi.org/10.2172/5986870.
Повний текст джерелаNye, C. J., R. J. Motyka, D. L. Turner, and S. A. Liss. Geology and geochemistry of the Geyser Bight Geothermal Area, Umnak Island, Aleutian Islands, Alaska. Office of Scientific and Technical Information (OSTI), October 1990. http://dx.doi.org/10.2172/6193109.
Повний текст джерелаIssler, D. R., K. Hu, L. S. Lane, and J. R. Dietrich. GIS compilations of depth to overpressure, permafrost distribution, geothermal gradient, and regional geology, Beaufort-Mackenzie Basin, northern Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2011. http://dx.doi.org/10.4095/289113.
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