Heat generation of basement rocks in the central part of the East European Craton
DOI:
https://doi.org/10.17308/geology.2021.3/3651Keywords:
East European Craton, Precambrian basement, heat generation of rocksAbstract
Introduction: We considered the general principles of creating complex geophysical models for the lithosphere of the central part of the East European Craton and the role of geothermal models in such models. In order to form a reliable initial estimate for a thermal model of the upper crust, we generalised the data on the content of heat generation elements in the rocks of the Early Cambrian basement. Initial data: We studied the peculiar features of the total content of rare and scattered elements obtained using the method of inductively coupled plasma atomic mass spectrometry in the samples of typical rocks of the studied region. A consolidated database was compiled for the content of heat generation elements (potassium, thorium, uranium) and the total content of silica in typical rocks of the crystalline basement of the craton. Assessment of heat generation of the basement rocks: We calculated the heat generation of the crystalline basement rocks in the area based on the initial data on the concentration of radiogenic elements. To assess the values of heat generation, we used the data on the density of the rocks of the basement of the East European Craton and its individual parts. The obtained results of the assessment of heat generation characterise the upper inhomogeneous part of the basement extending to the lower border of the region’s graviactive layer. Data analysis and discussion: We obtained the value of heat generation of the Early Cambrian basement rocks that varies from 0.1 to 7.54 μW/m3 with the average value of 0.528 μW/m3 . Data analysis showed that there was no correlation between the density of the region’s basement rocks and the calculated values of their heat generation. A stable connection was found between the content of silica (SiO2 ) and the value of the calculated heat generation of the rocks. As for the main groups of the basement rocks, heat generation tends to be related to the composition of the rocks, but there is no connection to the age of the formation of the rocks. Conclusions: We presented the main results of the conducted research and outlined a plan for the formation of an initial estimate for the heat generation of the upper crust in the thermal model of the region’s lithosphere.
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