The research of the structures of Mesozoic and Cenozoic basins of China should bebrought into the total pattern of the whole world,to dissect completely and deeply with theviewpoints of“mobilism”and“development stage”,and simultaneously to combine with thehistory of basin geotherm,sedimentary and structural evolution closely.
According to the corresponding relations in time and space between gold deposits and some aspects like uplift of Moho,deep faults,magma intrusions,aeromagnetic anomaly, gravity anomaly, circular structure and geotherm fields, the possibility of gold mineralization participated by deep fluid has been discussed.
The geothermal conductivity of sedimentary rock is an important parameter for geophysicists to analyse geothermal distribution and geothermal evolution in a sedimentary basin, and it is an essential factor which controls geotherm and geothermal flux in hydrocarbon basin.
Theinterlayer water and meteoric water were heated by geotherm, dynamic heat and heat released from metamorphosed organism to extract ore ma-terials from strata to form ore - bearing hot brine.
The studies of the allocation of tectonics, geotherm and coal metamorphic evolution indicated that to the Late Paleozoic coals in the east margin of the Ordos Basin, the preduction rate of coalbed methane is observably high and the time of gas generation is relatively centralized within the sections affected by abnormal geotherm of the Yanshan Period magma.
It has been widely applied in deep mother earth structure researching,oil and natural gas exploring,terrestrial heat field exploring , earthquake forecasting and researching.
The following is based on the analysis of the region's geothermy geologic conditions and the outcome of oil exploitation. Then the author puts forward detailed suggestions about the lay-out of well drillings and the design of the well drillings'structure.
Combined with the sedimentary burial history and basin geothermal history, the modeling of carbon isotope kinetics provides a new and effective means for the determination of the origin and accumulation history of natural gas pools.
The carbon isotopic characteristics of natural gas are not only affected by the gas source and maturity of the source rock, but also are related to the accumulation condition and geothermal gradient in a basin.
Several natural associations composed of thermophilic anaerobic bacteria capable of utilizing various cellulose materials at 60 ± 2°C and pH 6.0-7.0 were isolated from the sludge of Kamchatka geothermal springs.
It is assumed that a layer of mantle matter, rising up or going down, enters a region of decompression (in which for a number of reasons the geotherm passes above the temperature of the solidus) and is subjected to partial fusion there.
In basaltic composition, CaCO3 (calcite and aragonite), the major carbonate phase in marine sediments, is altered into MgCO3 (magnesite) via reactions with Mg-bearing silicates under conditions that are 200-300°C colder than the mantle geotherm.
Furthermore, CO2 itself breaks down to diamond and oxygen under geotherm conditions over 70?GPa, which might imply a possible mechanism for diamond formation in the lower mantle.
Temperature is an important factor affecting seismic velocity, and terrestrial heat flow is the most direct indication of temperature distribution of the lithosphere.
The problem under consideration is related to important engineering problems in hydrology, geothermy, as well as in the development of oil or gas fields [2-4, 5].
The heat in mine has a seriously harmful influence on the workers' health and excavation velocity, even can cause fire or bring significant loss when the mine flooding by hot water takes place. The heat source and type of heat-harm should be investigated before controlling it. For the hot water type heat harm, the dredging and drying measurements and strict managements should be taken with strengthening ventilation and using heat-resistant material. For the other types the improved conditions should be give...
Based on the water, mineral, geothermal, port and tourist geological resources as well as the engineering and environmental geolo- gical conditions of the country, the essay gives a full exposition of the influence and constraints of geological environment on the construction and development of China's open coastal cities and special economic zones.
In mine geothermal prediction, the instable heat transfer coefficient is an important parameter for heat transfer (between country rock and air flow) computation. In this paper the rock temperature distribution in the geothermal field has been presented. The analytic formula of the instable heat transfer coefficient has been derived, thus exponds the relationships between its nature and influencing factors. Practice showed that the analytic formula is accurate, simple and available.
地热
geothermal 
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