Interpretation of Thermal Measurements

摘要: Measurements of a number thermal parameters [e.g., temperature (T), the geothermal gradient (G or Γ), heat flow (Q q), generation (A H), conductivity (λ κ), capacity (c) and diffusivity (a)], interpretation measurements analysis regime different layers Earth (e.g., crust lithosphere) are among main tasks geothermics. Since (T) is one key used in thermodynamics, correct determination at any depth within where it cannot be measured an extremely important problem. Thermodynamic also for conditions preservation oil gas fields, as well such events metamorphism volcanism many other processes. The development model medium, methods analysis, problems absorption Earth's strata theory discussed. It shown that advanced developed magnetic prospecting may applied quantitative anomalies. Chapter finalized by considering models strongly nonlinear phenomena precursors earthquakes.