References
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Summary of heat flow studies in the Sohm abyssal plain: C.S.S. Hudson Cruise 80-016
Origin and history of the South China Sea Basin
Holocene paleotemperatures deduced from geothermal measurements
Forschungsvorhaben: Vertikalbewegungen und ihre Ursachen am Beispiel des Rheinischen Schildes
An inventory of geothermal resources in Nebraska
Heat flow in Bulgaria
An estimate of heat flow in the western north Atlantic at Deep Sea Drilling Project Site 534
Novo-Gvineyskoe (South Guinea Sea)
Teplovoe pole Timano-Pechorskogo neftegazonosnogo bassejna (Thermal field of the Timan-Pechera petroleum basin )
New heat flow data for the Romanian Territory
Contributo alla mappa del flusso geotermico in Italia: Misure dalle marche alla Puglia
State-coupled low temperature geothermal resource assessment program, fiscal year 1982. Final Technical Report
This report summarizes the results of low-temperature geothermal energy resource assessment efforts in New Mexico during the period from June 15, 1981 through September 30, 1983, under the sponsorship of the US Department of Energy (Contract DE-AS07-78ID01717). The report is divided into four chapters which correspond to the tasks delineated in the contract. Chapter 5 is a brief summary of the tasks performed under this contract during the period October 1, 1978, through June 30, 1983. This work extends the knowledge of low-temperature geothermal reservoirs with the potential for direct heating applications in New Mexico. The research effort focused on …
Leg 87 drills off Honshu and southwest Japan
Geothermal investigations in the Rhenish Massif
Heat flow from hydrothermal mounds in two million year old crust of the Mariana Trough which exceeds two watts per meter
Heat Flow Measurements
GEOTHERMAL GRADIENTS AND HEAT FLOW IN AUSTRALIAN SEDIMENTARY BASINS
Geothermal gradients in Australian sedimentary basins have been calculated from data obtained from water bores in the Great Artesian Basin and oil exploration wells. The data are subject to several types of systematic error, but statistical trends have been extracted , using values of thermal conductivity obtained from sediment compaction models . Estimates of heat flow from the Great Artesian Basin are consistent with the configuration of the major aquifer systems. Oil well data confirm the regional trends obtained from previous investigations, but previously recognised anomalies in southeast Australia are no longer evident. Temperatures at a depth of 40 kIn …