References

Nowcasting applications of geostationary satellite atmospheric sounding data Nowcasting

Heat flow in the Gulf Coastal Plain

Forty-four new heat flow values from panhandle Florida, southwestern Georgia, southern Alabama, Mississippi, and Louisiana range from 13 mW/m2 (0.3 HFU) (1 HFU = 1 ?cal cm?2 s?1 = 41.8 mW/m2) in Florida and Alabama to 88 mW/m2 (2.1 HFU) in northern Louisiana. In general, the values depict the eastern Gulf Coastal Plain as an area with low to normal continental heat flow that increases from east to west. Anomalously low heat flow (13?33 mW/m2) (0.3?0.8 HFU) characterizes north-central Florida, southwestern Georgia, and southern Alabama, while in northern Louisiana, 13 measurement sites yield values ranging from 50 mW/m2 (1.2 HFU) …

Geothermal investigations in West Virginia

New data on heat flow within the southeastern slope of the Kuramin Ridge

Terrestrial heat flow in the northwestern Pacific

On the basis of 150 new heat-flow measurements, the thermal structure of the uppermost layer of the Earth in the transition zone of the northwestern Pacific and relation of heat-flow values to the age of tectonic-magmatic activity, have been established. An analysis was made of the main factors distorting the geothermal field in the region under study, and a map of measured and background heat-flow values was constructed. Calculations were made to determine the temperatures in the deep crust and upper mantle along the DSS profiles in the northwestern Pacific, and a map was constructed showing the depth of the …

Thermal implications for the evolution of the spitsbergen transform fault

Heat flow taken between Svalbard and Greenland reveal three thermal provinces: 1.(1) the Molloy Ridge within the Spitsbergen Transform,2.(2) the Yermak Plateau3.(3) the northeastern margin of Svalbard (Nordaustlandet). The Molloy Ridge is a short spreading segment and the average heat flow is much above the Sclater et al. (1971), cooling curve but agrees with values from the Norwegian-Greenland Sea. An additional zone of intrusion identified by heat flow lies to the northwest of the Molloy Ridge. It straddles both the visible fracture zone and part of the Yermak Plateau. A thermal boundary lies between the warm western segment of the …

Estimates of terrestrial heat flow in northern Chihuahua, Mexico, based upon petroleum bottom-hole temperatures

A detailed study of the distribution of heat flow and radioactivity in New Hampshire (U.S.A.)

New determinations of heat flow in Siberia

An appraisal of Australian heat-flow data

Baja California passive margin transect; Sites 474, 475, and 476

Guaymas Basin slope; Sites 479 and 480

Guaymas Basin; Sites 477, 478, and 481

Teplovoe pole mestorozhdeniya akchatau, zentralni Kazakhstan. (Thermal field of the Akchatau field, central Kazakhstan)

Preliminary study on geothermal gradient and heat flow in Java

Evidence of form higher temperatures from alteration minerals, Bostic 1-A Well, Mountain Home, Idaho

The Winona Basin: structure and tectonics

Heat-flow measurements at shot points along the 1978 Saudi Arabian seismic deep-refraction line, part 2: discussion and interpretation

Geotermija Bajkala (Geothermy of Baikal )

Principles of temperature mapping

Temperature mapping can be performed by observing temperatures at different depths and by calculating mean gradients for the fo rmations. Temperatures are calculated between wells by using surface temperature and interpolated mean gradients for each formation. Basicly this principle differs from usual technique by using interpolation of mean gradients instead of interpolating mean conducti vi ty and heat flow . In cases where interpolation of gradients are impossible due to in sufficient data the gradie nts can be found by using the relations of the mean gradients fo r sedimentary sequences. Measurements of conductivity on core samples wi ll contribute …