References
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Ege Bolgrsinde Jeotermik Arastirmalar
Vertikal'nye variacii teplovogo potoka na Juzhnom Urale (Vertical variations of heat flow in the South Urals )
The thermal regime of the crystalline continental crust: Implications from the KTB
An extensive geothermal research program within the German Continental Deep Drilling Program (KTB) covered an almost complete spectrum of experimental and theoretical aspects. The main results and conclusions are as follows: (1)Equilibrium temperature is 118.6 degrees C at 4000 m in the KTB pilot borehole (KTB-VB) and will be around 260 degrees C at 9100 m in the KTB main borehole (KTB-HB). Time required for thermal equilibration of the KTB-HB to within 1% of the initial perturbation will be about 13-16 years. (2) The failure to predict temperature correctly for the KTB was mainly due to an unaccounted perturbation by …
O popravkah k eksperimental'nym ocenkam glubinnogo teplovogo potoka (On corrections to experimental estimates of deep heat flow )
Heat flow of the Northwest Pacific
Heat Flow Map of East and Southeast Asia
Resistivity and Heat Flow Studies at Mae Chan Geothermal Area, Chiangrai Province
Heat flow in the Cretaceous of Northwestern Kansas and implications for regional hydrology
Heat flow across the East African Plateau
Four new heat flow measurements from western Tanzania are combined with existing data from non-rifted areas of East Africa to determine if there is a broad heat flow anomaly associated with the East African Plateau. Three of the new data sites lie in the Kibaran Belt and yield heat flows of 60, 68, and 74 mW m(2), The fourth new site is in the interior of the Tanzania Craton and gives a heat flow of 33 mW m(2). The ensemble of heat flow data from the interior of East Africa, when compared to the global distribution of heat flow in …
Teplovoj potok Sahalina i Juzhnyh Kuril'skih ostrovov (Heat flow of the Sakhalin and the South Kuril islands )
Paleotemperature gradient and thermal history of Tulufan-Hami Basin,Xinjiang
Thermal regime of the San Andreas fault near Parkfield, California
Knowledge of the temperature Variation with depth near the San Andreas fault is Vital to understanding the physical processes that occur within the fault zone during earthquakes and creep events. Parkfield is near the southern end of the Coast Ranges segment of the San Andreas fault. This segment has higher mean heat flow than the Cape Mendocino segment to the northwest or the Mojave segment to the southeast. Boreholes were drilled specifically for the U.S. Geological Survey's Parkfield earthquake prediction experiment or converted from other uses at 25 sites within a few kilometers of the fault near Parkfield. These holes, …
Estimates of conductive heat flow through bottom-simulating reflectors on the Hikurangi and southwest Fiordland continental margins, New Zealand
Bottom-simulating reflectors (BSRs) represent the base of the stability field for gas hydrates in shallow oceanic sediments. A simple conductive model is used to calculate surface heat flow through the Hikurangi and southwest Fiordland continental margins of New Zealand, based on the depths of BSRs. The results indicate mean uncorrected heat flows through the two regions of 37 +/- 8 mW m(-2) and 40 +/- 9 mW m(-2), respectively. Corrections to the Hikurangi data for the effects of late Neogene sedimentation give an estimate of the true mean heat flow of 44 +/- 10 mW m(-2), in agreement with values …
Thermal Structure and Tectonic History of the Derugin Basin, Sea of Okhotsk (in Japanese with English abstract)
El'nikov AI Ocenki teplovogo potoka na ozere Bajkal po sejsmicheskim dannym o nizhnej granice sloja gazogidratov (Estimates of heat flow at Lake Baikal from seismic data on the lower boundary of the gas hydrate layer )
Teplovoj potok i radiogennaya teplogeneraciya na Yuzhnom Urale (Heat flow and radiogenic heat generation in the Southern Urals )
Prospeccion geofisica para la evaluacion del potencial geotermico del sector norte del Valle de la Laguna Salada
Variations in heat flow across the ocean-continent transition in Iberia abyssal plain
New heat flow observations have been made in the Iberia abyssal plain off the Galicia margin along the transect of Ocean Drilling Program Leg 149 drill sites, in order to investigate the nature of this unusually wide and deep continent-ocean transition region. Our results indicate the presence of three separate zones. Average values of 47.5 ± 3 mW m−2 in the westernmost zone III agree with predictions of standard oceanic lithospheric models for its estimated age of 126 Ma. In contrast, the heat flow within zone II is 5–15 mW m−2 higher than predicted, assuming that the mantle heat flow …