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.
Terrestrial heat flow in eastern Slovakia
Tepelný tok ve vrtu NV-1 - Nová Ves u Chýnova (Heat flow in the borehole NV-1)
Heat flow in the Snowy Mountains of Australia
Heat flow in the Snowy Mountains has been calculated from the underground temperatures taken during the construction of five major tunnels enclosing an area of about 1000 km². Four of the tunnels are in reasonably homogeneous granitic rocks for appreciable portions of their lengths, and reliable heat flows could be obtained from the parts of the tunnels in this type of rock. Measurements of the thermal conductivity of a total of 161 specimens were used in the calculations of the heat flows. The results in these four tunnels, based on 124 temperature measurements corrected for the influences of the surrounding …
Thermal conductivity of rocks and its measurement with the divided-bar apparatus
Heat flow in the Kladno-Rakovnik coal basin
The measurement of terrestrial heat flow in the Mecsek Mts
On some geothermal flux determinations in France (Sur quelques déterminations de flux géothermique en France)
Il flusso geotermico sotto il Monte Bianco
Terrestrial heat flow in Hungarian Permian strata
Studies of the thermal state of the Earth. The 21st paper: Heat-flow, Eastern Pacific
Terrestrial heat flow in Khetri Copper Belt, Singhbhum Thrust Zone and Godavari Valley, India
On heat flow in Iceland in relation to the Mid-Atlantic Ridge
Terrestrial heat flow in Khetri copper belt Rajasthan, India
Terrestrial heat flow in Lake Malawi, Africa
Twenty measurements of heat flow through the floor of deep Lake Malawi (Central Africa) gave values ranging from 0.15 to 2.88 ?cal/cm² sec. A systematic areal distribution of the values indicated regions of low heat flow at the northern and southern ends of the lake (average = 0.54 and 0.70 ?cal/cm² sec, respectively), separated by a central region of high heat flow (average = 2.30 ?cal/cm² sec.). The variability implies local heat sources within a few tens of kilometers of the earth's surface and/or disturbances from the local environment.