2019
DOI: 10.1088/1755-1315/249/1/012042
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Evolution in information on crustal geothermal parameters due to application of advanced experimental basis

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Cited by 2 publications
(10 citation statements)
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“…Spatial and temporal variations in HFD are derived from a geologically constrained model or, less commonly, from simplified analysis, i.e., using the McKenzie model (McKenzie, ) or its modifications in the case of extensional basins. Regardless of the approach, specialists rely on present‐day HFD maps, which frequently involve significant errors (Popov et al, , ). Moreover, HFD geohistory is sometimes locally modified during calibration, which leads to variations in temperature/maturity without proper geological justification.…”
Section: Pitfalls Of the Customary Approach To Geothermal Characterizmentioning
confidence: 99%
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“…Spatial and temporal variations in HFD are derived from a geologically constrained model or, less commonly, from simplified analysis, i.e., using the McKenzie model (McKenzie, ) or its modifications in the case of extensional basins. Regardless of the approach, specialists rely on present‐day HFD maps, which frequently involve significant errors (Popov et al, , ). Moreover, HFD geohistory is sometimes locally modified during calibration, which leads to variations in temperature/maturity without proper geological justification.…”
Section: Pitfalls Of the Customary Approach To Geothermal Characterizmentioning
confidence: 99%
“…Our long‐term experience (1985–1991, 1996–2014) of geothermic research in unique deep and superdeep continental scientific wells in former USSR, Germany, USA, Mexico, etc. with numerous temperature measurements in wells and more than 30,000 samples investigations (Popov et al, ) shows that (a) vertical HFD variations must be recorded, (b) heat generation has little effect compared with the influence of paleoclimate (tens of percent), fluid migration in the well and the effects of averaging of the thermal gradient, (c) the results are distorted due to systematic errors in the use of traditional contact methods of thermal conductivity measurements, the neglect of anisotropy, the small volume of the core under study at a substantial heterogeneity of the sections. The neglect of the above factors does not allow registering significant local variations and the general trend of heat flow along the wells.…”
Section: Pitfalls Of the Customary Approach To Geothermal Characterizmentioning
confidence: 99%
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