Titlebook: Geothermics and Geothermal Energy; Ladislaus Rybach,Lajos Stegena Book 1979 Springer Basel AG 1979 earth science.energy.engineering.geolog

archaeology

Infusion

The Degree of Metamorphism of Organic Matter in Sedimentary Rocks as a Paleo-Geothermometer, Appliedganic matter increases continually. Apart from temperature, the slowly reacting chemical compounds of the organic matter strongly depend on time, too..It is shown that the coal rank is proportional to the integral of temperature and time of burial (.) for the Tertiary sedimentary rocks of the Upper

Aqueous-Humor

The Preliminary Heat Flow Map of Europe and Some of its Tectonic and Geophysical Implications temperatures, gradients and local heat flow patterns. In areas without data the heat flow field was extrapolated on the basis of the regional tectonic structure and the observed correlation of heat flow and the age of the last tectono-thermal event. The heat flow pattern as obtained in the map may

Meager

alabaster

Mantle Heat Flow and Geotherms for Major Tectonic Units in Central Europeeneration models for the crust in the Paleozoic Platform region, the Sudetic Mountains (Variscan Internides) and the European Precambrian Platform show considerable differences in mantle heat flow and temperatures. At the base of the crust variations from 440–510°C in the models of Precambrian Platf

凹槽

On the Geothermal Regime of Some Tectonic Units in Romania0–120 mW m. for the Neogene volcanic area. Temperature-depth profile and some geophysical implications of the low values for the Transylvanian Depression are discussed, rendering evident clear-cut differences between this tectonic unit and other Neogene depressions. The heat flow values for the othe

宮殿般

Heat Flow in Italygeological features with the following results: foreland areas, 55+19 mW m., foredeep areas, 45 ± 21 mW m .; folded regions and intermountain depressions, 76 ± 29 mW m.. In volcanic areas the heat flow rises to in excess of 600 mW m.. From a tectonic point of view, these values are consistent with t

choleretic

啟發(fā)

Geothermal Resource Assessment of the United Statest some reasonable future time. In the United States, the Geological Survey is responsible for preparing geothermal assessments based on the best available data and interpretations. Updates are required every few years owing to increasing knowledge, enlarging data base, improving technology, and chan

emission