1887

Abstract

On the base of variation finite element method for non stationary three dimensional heat conductivity model with calculation of the oceanic lithosphere layers heterogeneity and oceanic crust radiogenic heat emission, and also with calculation of the ocean and asthenosphere heat irradiations there were obtained oceanic lithosphere heat fields during it cooling process. The obtained results allowed to specify heat fields and power of the oceanic lithosphere data, during it cooling process, which were obtained earlier on the base of more simple heat conductivity models.

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/content/papers/10.3997/2214-4609.20140403
2014-05-12
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20140403
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