References
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Heat flow near the South Atlantic Triple Junction, 55°S, 0°E
Geothermal studies Leg 31
Rezul'taty opredelenija glubinnogo teplovogo potoka na territorii Jakutii (Results of determining the deep heat flow in Yakutia )
Bituminous Indications in the Roblin RO-1 borehole in the Barrandian, to the SW of Prague
Temperature Phenomena and Heat Flow Estimates in Two Precambrian Ore-bearing Areas in North Sweden
Temperature measurements in 17 drillholes reaching vertical depths between 365 and 780 m below ground surface in the Skellefte area (lat. 65° 52deg;N, long. 20° 20° E Gr) and Aitik area (lat. 67° 5deg;N, long. 21° E Gr) in the Swedish precambrian are reported. The absolute accuracy of the measurements was about 0·03°C and the relative one about 0·005°C. A large number of thermal diffusivity measurements were made on rock samples from the two areas in order to estimate the correction to the observed steady geothermal gradients due to climatic amelioration at the end of the Pleistocene. The corrected gradients …
Geothermische Messungen in der Bohrung Bad Sassendorf
Late Cenozoic evolution of the Pannonian basin
The Palaeozoic—Mesozoic nucleus of the Pannonian basin is the result of the collision of the European and Gondwanic microplates. The present basin was formed in the Late Cenozoic by the subsidence of this nucleus. The sinking was brought about by an active mantle diapir which was generated by the subduction associated with the formation of the surrounding mountains. The evidence and consequences of the mantle diapir are as follows. 1.(1) Strong Miocene andesitic-rhyolitic and Plio-Pleistocene basaltic volcanism.2.(2) Geothermal highs and the high value of reduced heat flow (Qo = 1.2−1.7 HFU).3.(3) Anomalous upper mantle with a lower density and elevated …
Bottom water flow through the Kane Gap, Sierra Leone Rise, Atlantic Ocean
Geotermicheskie issledovanija v glubokovodnoj chasti Vostochno-Kitajskogo morja (Geothermal research in the deep-water part of the East China Sea )
Terrestrial heat flow studies in Kenya
Heat flow determination during the second complex ocean expedition of the Sakhalin Complex Scientific Research Institute
Porosity determinations and the thermal conductivity of rock fragments with application to heat flow on Cyprus
A standard core analysis technique has been modified to estimate porosities from measurements on rock fragments. For the range of rocks tested, chip-determined fractional porosities were within ±0.025 of the values measured on solid-core samples. This has enabled thermal conductivity measurements on rock fragments to be corrected for the effect of porosity, yielding agreement with conductivity determinations on solid core generally to better than ± 10%. The application of this is illustrated by the determination of heat flow in a 300-m borehole in western Cyprus (latitude 34°54′N, longitude 32°34′E, elevation 82 m). A decrease in temperature gradient with depth is …
The Marysville Geothermal Area, Montana
A heat flow study in the Turtle Lake quadrangle, Washington
Terrestrial Heat Flow along the Rio Grande Rift, New Mexico and Southern Colorado
From heat-flow data obtained in New Mexico and southern Colorado, we recognize (1) a major geothermal anomaly with heat-flow values greater than 2.5 HFU (heat-flow unit, µcal/cm2-sec) coincident with the western part of the Rio Grande rift, (2) a complex heat-flow pattern in the eastern Colorado Plateau with values of 1.5 HFU and less, apparently associated with major structural basins, and values of 2.0 HFU and greater, apparently associated with some intrusions and perhaps major uplifts, (3) a regional increase in heat-flow values from 1.5 to 2.0 HFU to values greater than 2.5 HFU in southwestern New Mexico, which may …
Glomar challenger returns to the mediterranean sea
Heat flow through the Southern California Borderland
Geotermicheskie Usloviya Severnoi Chasti Pri- Pyatskoi Vpadiny (Geothermal conditions of the northern part of the Pripyat Depression )
Terrestrial heat flow near Datil
Terrestrial heat flow in the neogene foredeep and the flysch zone of the Czechoslovak Carpathians
All available heat flow data together with temperature gradients and thermal conductivities of rocks from deep holes in the area forming the contact zone between the Bohemian massif and the western Carpathians are summarized. These data include 20 previously published values and 12 new values. The technique of measurement of the underground temperature, as well as the laboratory determination of the coefficient of thermal conductivity is briefly described. The most important result is the increase of the geothermal activity along the Carpathian foredeep from the south to the north and the generally high heat flow in the area of Permo-carboniferous …