References
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Interpretation of heat flow data in the French Massif Central
We investigate in this paper the possible origin of the high heat flow anomaly observed in the Massif Central (100–110 mW m−2). A detailed study of crustal heat production shows that the radioactive component cannot account for the entire surface anomaly. However, when we remove the integrated radioactive contribution from the surface heat flow, it appears that the anomaly is reduced to a smaller area close to the Cenozoic graben and the volcanic area, with an amplitude of 25–30 mW m−2. This mantle heat flow anomaly is interpreted as a transient component related to a mantle diapir ascent in the …
O Svyazi Teplovogo Potoka S Geologicheski- Mi Strukturami DNA Severnogo Ledovitogo Okeana - V Kn: Teoreticheskie I Experimentalnye Issledovaniya Po Geotermike Morey I Okeanov Moskva: Nauka, (About the Connection of Heat Flow With Geologically Mi Structures of the DNA of the Arctic Ocean)
High heat flow in southern Tibet
HEAT FLOW AND GEOTHERMAL GRADIENT STUDIES IN THE ALBERTA BASIN AN ESSENTIAL PART OF GEOTHERMAL POTENTIAL EVALUATION
ABSTRACT Geothermal gradients in the Alberta part of the prairies basin in Canada have been studied on the basis of 55,246 bottom-hole temperature values from 28,260 petroleum exploration wells. Gradient estimates for different depth and stratigraphic intervals together with the study of the heat conductivity distribution have provided knowledge of both regional heat flow variations and heat flow variations with depth. It is found from the study that both regional and depth variations of grad T and heat flow are influenced by the regional hydrodynamics of the basin. The geothermal gradient and heat flow tend to increase with depth in …
Rezul'taty geotermicheskikh issledovaniy na Pamire (Results of geothermal research in the Pamirs)
Heat flow density determination in the Strymon basin, NE Greece
Heat flow studies in geothermal prospect areas of japan
Terrestrial Heat Flow Determinations In Central Kyushu, Japan
The thermal structure and thermal evolution of the continental lithosphere
For thermal considerations, the lithosphere is defined as the outer layer of the Earth in which heat transfer is dominated by conduction. Low density continental crust caps the continental lithosphere preventing its subduction, and thus it has, in general, a long and complex thermal history. The thermal regime in the near surface zone of the continental lithosphere is commonly complex, and is responsible for much of the scatter in shallow heat flow data, the main data set used to examine the thermal structure and evolution of the continental lithosphere. A review of continental heat flow data shows that while heat …
Thermal regime of the continental lithosphere
Thermally, the lithosphere may be defined as that outer portion of the earth in which heat is transferred primarily by conduction. It generally includes the crust and part of the mantle. The thermal regime of continental lithosphere is determined by many factors including heat flow from the asthenosphere, the vertical and lateral variation of both thermal conductivity and radiogenic heat production, tectonic history, and such superficial processes as climatic history and the shallow hydrothermal regime. From studies of the global heat flow data set, two generalizations regarding continental lithosphere have arisen, namely that: 1) there is a negative correlation between …