References
This section lists all references that have been added to this portal. You can search and filter references by type, author, title, and other metadata. Each reference may include a DOI, publication date, and other relevant information to help you find and cite the literature effectively.
Crustal Structure of Iceland from Explosion Seismology
Five Measurements of Heat Flow in Southern Canada
Geothermal heat flux evaluated from turbulent fluctuations above the sea floor
Heat flux values measured in the sediment with a 2.5-meter Bullard probe agreed with the values determined from spectra of temperature and current measured in the water within a meter of the ocean bottom. This agreement, together with the absence of significant long-term temperature fluctuations in the abyssal water, suggests that above-bottom heat flux measurements may be practical.
Measurements of terrestrial heat flow in Hokkaido (Part 2)
Terrestrial Heat Flow in Hokkaido, Japan : Preliminary Report
Bericht über geothermische Messungen in der Bohrung Weissenstein
Heat flow in the western United States
Elevation of ridges and evolution of the central eastern Pacific
An empirical relationship between ridge elevation and age of the oceanic crust is presented for the Pacific, Atlantic, and Indian oceans. This relationship is accounted for by the thermal contraction of a cooling lithosphere as it moves away from a center of spreading, and thus is compatible with plate theory. Hence, it is possible to use topographic profiles to predict the age of the ocean floor. Detailed examination of profiles in different areas indicates that slow-spreading ridges (half-rate <3 cm/yr) may have a shallower crestal elevation than faster ridges (half-rate >3 cm/yr). However, all ridges appear to show a …
Lake Tanganyika: water chemistry, sediments, geological structure
Bericht über geothermische Messungen in der Bohrung Riedenburg
Sea floor geothermal measurements form Vema cruise 24
Thermal conductivity of rocks from measurements on fragments and its application to heat-flow determinations
A series of measurements indicates that the thermal conductivity of a rock generally can be estimated adequately for geophysical purposes from simple laboratory measurements on fragments of the rock. The solid-rock conductivity is deduced from a divided-bar measurement of the conductivity of a cylindrical cell containing water-saturated rock fragments. All determinations fall within about ten per cent of conventionally measured solid-rock values for a variety of crystalline and sedimentary rocks with conductivities ranging from about 3 to 14 mcal/cm sec°C. Good agreement is found between values determined from drill cuttings and solid core from the same depth in deep boreholes. …
Geothermal measurements on Leg 8
Heat Flow through the Floor of the Cascadia Basin
Measurements of Terrestrial Heast flow in Hokkaido (Part 2)
Teplovoe pole Ukrayiny (Thermal Field of Ukraine )
Veplovye Potoki I Neftegazonosnost Na Primere Dono-medveditskoi Sistemy Dislokatsii (Heat flows and oil and gas content on the example of the Dono-Medveditskaya Dislocation System )
Eine neue Methode zur Bestimmung der terrestrischen Wärmestromdichte in Binnenseen
Die Dichtc des terrcstrischen Wiirmestromes kann aus Messungcn in den Lockcrsedimenten am Boden von Binnensccn ermittelt werden, wenn die MeBstelle in min- I i' destens SO m Wassertiefe liegt und wenn man die Messungen im Herbst durchnihrt. Diese Bedingungen ergeben sich aus einer Betrachtung der raumzeitlichen TemperaturverteiIung ' im Wasser von Binnensecn. An den Ergebnissen ist im wescntlichen noch eine Korrektur I anzubringen wegen der durch den See hervorgerufenen Stiirung des Tempcraturfeldes im Boden. Der Gesamtfehler der Methode wird auf ±20% oder kleiner geschiitzt. I Urn diese Moglichkeit uuszunutzen, wurde eine Sonde gebaut, mit der folgende GroBen gemessen werden konnen: …