References
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Heat flow in the vicinity of the Mount Hood volcano, Oregon
Temperature data from the Mexico drilling area: report on logging and inhole temperature experiments
Geothermal measurements in the southern Appalachian Mountains and southeastern Coastal Plains
Assessment of Geothermal Resources of Brazil
Terrestrial heat flow in Arizona
New heat flow data in Arizona suggest that the southern Basin and Range has recently undergone less extension than other areas of the Basin and Range province. Heat flow?heat production data imply that magmatism and hydrothermal circulation in the crust and upper mantle beneath southern Arizona and northwestern Mexico may be less extensive than along the Rio Grande rift. A heat flow transition between the Basin and Range and the Colorado Plateau occurs within a lateral distance of 60 km in central Arizona. Predicted steady state temperatures suggest that the M discontinuity may be nearly coincident with an isotherm along …
Gravity and thermal models for the Twin Peaks Silicic Volcanic Center, southwestern Utah
Gravity, heat flow, and surface geology observations have been used as constraints for a thermal model of a late Tertiary silicic volcanic center at Twin Peaks, Utah. Silicic volcanism began in the area with the extrusion of the Coyote Hills rhyolite 2.74 ± 0.1 m.y. ago, followed by the Cudahy Mine obsidian, felsite, and volcanoclastics, and finally by a complex sequence of domes and flows that lasted until 2.3 ± 0.1 m.y. ago. Basalt sequences span the time 2.5 to 0.9 m.y. Terrain-corrected Bouguer gravity anomalies at Twin Peaks are shaped by three features of varying characteristic dimensions: (1) a …
A heat flow survey on anomaly M0 south of the Bermuda Rise
Heat Flow Measurement
Down-hole temperature measurements and heat flow at Hess Rise, Deep Sea Drilling Project Leg 62
Present heat flow and a preliminary paleogeothermal history of the central prairies basin, Canada
The heat flow pattern in the Prairie Basin in Canada is influenced mostly by hydrodynamic conditions in the deep geological strata. The hydraulic head is a post-Laramide feature and the exceptionally high heat flow values in the Prairies are closely related to the upward fluid motion in the porous formations. Heat flow values in the Prairies are higher than in other Precambrian platforms in the world. On the basis of coal maturation studies it can be shown that the paleo-geothermal gradients were slightly lower in the Central Prairies during Eocene-Oligocene times than those observed at present. The maximum burial temperatures …
Regional heat flow patterns in the Western Canadian Sedimentary Basin
The regional geothermal pattern of the Western Canadian Sedimentary Basin has been studied using available temperature data from wells. Average heat conductivity for various geological formations has been estimated on the basis of net rock studies by Canadian Stratigraphie Services. These data and observations of temperature made in “shut-in holes” in some of the oil pools have been used in heat flow estimations by the Bullard method. The geothermal gradient and heat flow within the basin are exceptionally high in comparison with the other world wide Precambrian platform areas. Especially high geothermal gradient areas are found in the northwestern part …