References
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On the geothermal regime of Transylvanian Depression
Geothermal profile in the Central Moesian Platform
An active spreading center collides with a subduction zone: A geophysical survey of the Chile Margin triple junction
The triple junction between the Nazca, Antarctic, and South American crustal plates has been mapped at lat 46.4°S, long 75.7° W. The Chile Ridge, an active spreading center opening at a half-rate of 28 mm/yr, can be traced into the axis of the Chile Trench; at the triple junction itself, the axial rift valley abuts the inner wall of the trench. The spreading process does not appear to be modified by proximity to a subduction zone until the actual point of collision: magnetic anomalies formed by sea-floor spreading can be traced to the inner wall of the trench; the depth …
Misure di flusso di calore nei mari italiani: stato di avanzamento della Ricerca
Flux de chaleur, production de chaleur et évolution géodynamique récente du Massif Central français
Investigations of low-temperature geothermal potential in New York State
Heat-flow studies in Wyoming, 1979 to 1981
Calculation of terrestrial heat flow solely from oil well logging records
Preliminary heat-flow measurement at the Illinois deep drill hole
Evolution tectonique et sédimnetaire du Bassin Ligure, Mediterranée occidentale
New Mexico State University campus geothermal demonstration project: an engineering construction design and economic evaluation. Final technical report, February 25, 1980-April 24, 1981
Geotermicheskaya kharakteristika osadoch- nykh otlozhenii i teplovoi potok v raione g minska - doklady an bssr 1981 (Geothermal characteristics of sedimentary deposits and heat flow in the area of Minsk )
Mechanisms of heat transport through the floor of the equatorial Pacific Ocean
Thermal structure of the yakedake volcano, Japan: Karukaya and Takara geothermal areas
The hydrothermal water balance and the thermal structure of Yakedake volcano and its vicinity are considered quantitatively. The hydrothermal activity is intense in the valleys at the western foot of the volcano and the Nakanoyu area. The total hot water flow from the discharge area amounts to 2.07 × 1041/min, about 60% of which discharges from the Shinhodaka area alone. There are some large basins (Abodaira and others) in which the rocks are mainly tuff breccia and volcanic products showing very high permeability for water. The total area of the water recharge zone amounts to 18.2 × 106m3. A model …
Temperature measurements in oil wells
Measurements of thermal conductivity of drill cuttings in the Marchwood geothermal borehole — a preliminary assessment of the resource
Heat flow study in the oil basinal areas in Indonesia
The subsidence, Thermal and maturation history of the Pattani Through in the Gulf of Thailand
Simple models of diffuse extension and the pre-seafloor spreading development of the continental margin of the north-eastern Gulf of Aden
Heat flow and geothermal assessment of the Escalante Desert, southwestern Utah, with emphasis on the Newcastle KGRA
Twenty-five new regional heat flow measurements are presented for the Escalante Desert region within the Great Basin of the western US. Heat flow excluding geothermal areas ranges from 42 to 350 mW m/sup -2/ but much of the variability may be caused by deeply circulating groundwater redistributing the regional flux. A subset of 10 sites drilled specifically to characterize the heat flow of the region yielded a mean of 100 mW m/sup -2/ with a standard deviation of 22 mW m/sup -2/. An analysis of thermal conductivities of solid cylindrical discs and rock chips of rhyolite to andesite tuffs emphasized …