the European climate
the Sitemap
Two-dimensional anomalies of heat conductivity
illegitimacy Consequences
the Refraction of a thermal stream
the Previous works
the Numerical method
Models
Results and discussion
Models l1
Models l2 and l3
Model f
the Conclusion
the Analysis of a superficial thermal stream
Features of a thermal field evropy
the Method of modelling calculations
Results of modelling calculations
Interpretation
Explosive tectonics and a thermal field evropy
Tectonic ruptures
Types of ruptures and their arrangement
the Arrangement of ruptures
Tafrogennye structures
the Mediterranean
Depth of system of ruptures
the Thermal stream and an arrangement of ruptures
the East European platform
the Average europas
Structures grabenov
the Mediterranean area
the Thermal stream, capacity of a bark
Geophysical interpretation of modern movements
Movements of earth crust of average evropy
the Thermal stream and vertical movement
the communication Analysis
Capacity of a bark
the Caucasian region
Conclusions
Value of researches of a thermal stream
the General theoretical remarks
the Volume specific thermal capacity
Process of allocation of heat
Types of geothermal deposits
Liquid geothermal deposits
Steam geothermal deposits
Hydrothermal konvektivnye systems
Blocking breeds
the Average temperature gradient
Deposits with low entalpiej
Systems of hot magma
Impenetrable systems
Breeds with it is abnormal high plastovym pressure
Geothermal data on bolgarii
Geological structures
the Thermal field and tectonic elements
the Mizijsky plate
the Tectonic zone Balkan forlanda
Sredna-mountain
the Picture rodopskogo a file
Northeast rodopskaja depression
the Thermal stream in velikobritanii
Measurements of a geothermal gradient
Definition of factor of heat conductivity
Measurements of a temperature gradient
Factors of value of temperature gradients
Heat conductivity
Results
the Analysis of results
geotermija vengrii
Thermal sources
Geology and region hydrogeology
Verhnepannonsky adjournment
the Pannonsky hollow
Geothermal data
Standard definitions of a thermal stream
Measurements of a thermal stream
Value of a thermal stream
the Estimation of a thermal stream
Meteorological stations
temperature Cards
Sizes shtegeny
Map development of a thermal stream
the Result
Tektonofizika pannonskogo a maximum
Features
the Field of a thermal stream in territory gdr
Anomalies of a thermal stream in gdr
Stations of a thermal stream
Measurements of a thermal stream frg
Available data
the Card of a thermal stream and its interpretation
Feature of a thermal field
the Analytical method
the Preliminary card of a thermal stream gretsii
New data
the Card of a thermal stream gretsii
the south Review
Northern part egejskogo the seas
Geophysical features of region gretsii
Discussion
Increase in a thermal stream
the Greatest depth of immersing of a plate
Anomaly of a thermal stream
the Thermal stream in danii
the Thermal stream and deep temperatures
bark Structure
Data of deep seismic sounding
Deep temperatures
heat conductivity Factor
Use of two probes
the Collection swept also limestone
Estimations of a thermal stream
Boreholes
the Simplified model
Discussion and conclusions
the highest korovye temperatures
Negative correlation
Konduktivnyj a thermal stream in islandii
the Summary
Temperature gradients
Data on southwest islandii
Temperature a gradient in ispanii
the Thermal stream
an earth crust Structure
Temperatures in earth crust
the Thermal stream in italii
the Technique
Data about a thermal stream
Data about a thermal stream (ii)
Character of distribution of a thermal stream
Apenninsky peninsula and sitsilija
Volcanic adjournment
Values of a thermal stream
the Ligurijsko-Tuscan arch