Literature Review
The Global Heat Flow Database (GHFDB) is committed to maintaining the highest standards of data quality. To achieve this, we have implemented a rigorous literature review process that ensures all datasets are thoroughly vetted before being made publicly available. To learn more about the review process and how you can contribute, please click the button below.
CU PRIVIRE LA EFECTUL LUCRARILOR DE FORAJ ASUPRA CAMPULUI TERMIC NATURAL (ON THE EFFECT OF BORE HOLE DRILLING ON THE THERMAL FIELD OF THE AREA)
A compilation of Australian heat-flow measurements
DETERMINAREA CONDUCTIVITATII TERMICE A ROCILOR PRIN MASURATORI DE FRAGMENTE DE ROCA (DETERMINATION OF THERMAL CONDUCTIVITY OF ROCKS FROM MEASUREMENTS ON FRAGMENTS)
Heat Flow Measurements In Hungary
Heat flow, heat production and crustal dynamics in the central Alps, Switzerland
Geothermal measurements in Palaeogene, Cretaceous and Permocarboniferous sediments in northern Bohemia
Method for determining terrestrial heat flow in oil fields
Heat flow in Florida oil test holes and indications of oceanic crust beneath the southern Florida- Bahamas platform
Climatically perturbed temperature gradients and their effect on regional and continental heat-flow means
Investigation of the S.W. England thermal anomaly zone
Heat flow measured over the Juan de Fuca Ridge: Evidence for widespread hydrothermal circulation in a highly heat transportive crust
Das Geothermische Feld des Rieses (About the geothermal field of the Ries)
Kurzfassung Die Ergebnisse von Temperaturmessungen in den Bohrungen Fabrik Busse, Malzfabrik Nördlingen, Deiningen l, Wörnitzostheim und Nördlingen 1973 werden zusammenfassend dargestellt. Für die Temperaturgradienten ergeben sich folgende Werte (in °C/100m): Seetone 8,4; Suevit 3,9; großblockige kristalline Trümmermassen 3,2. Die Wärmestromdichte im Rieskrater berechnet sich unter Berücksichtigung der geringen Wärmeleitfähigkeiten der Gesteine des Rieskörpers zu 1,75 HFU (73,2 mW nr2) für den Bereich der Bohrung Nördlingen 1973 und zu 1,93 HFU (80,7 mW m-2) für die Bohrung Wörnitzostheim. Diese Werte entsprechen dem im Untersuchungsgebiet erwarteten Wert von 1,8 HFU. Summary Temperature measurements carried out in the drillholes Fabrik Busse, Malzfabrik Nördlingen, …
Review of heat flow data from the Mediterranean and Aegean Seas
A composite trans-Atlantic heat flow profile between 20° and 35°
Geothermal gradients in British lake sediments
Heat Flow in Back-Arc Basins of the Western Pacific
Summary A review of heat-flow data in trench-island arc and back-arc basins of the Western Pacific shows that for basins associated with current subduction at a trench, profiles of heat flow normal to tectonic trends have common features: 1) the zone from the trench axis to the volcanic zone has below average heat flow; 2) the volcanic zone has high but variable values; and, 3) the back-arc basins have mean heat flows that depend on age. Basins younger than Miocene have high heat-flow values. Scattered very low values suggest that water circulation within the young oceanic crust may be a …
Neposredstvennye izmereniya teplovogo potoka iz nedr Zemli v skvazhinah (Direct measurements of heat flow from the Earth’s interior in boreholes )
Two heat flow values for Tasmania
The terrestrial heat flux was determined at two sites in Tasmania. At Glenorchy (147° 15′ E, 42° 50′ S) it was 87 mWm−2 in a dolerite section centred at 350 m depth. At Olga Ridge (145° 47′ E, 42° 46′ S) it was 57 mWm−2 in a mudstone section centred at 250 m.