Radiogenic heat production variability of some common lithological groups and its significance to lithospheric thermal modeling
By M. Vilà, Manel Fernàndez, I. Jiménez‐Munt. 2010
226 citations recorded by the source corpus.
Subfields: Geophysics, Radiological and Ultrasound Technology
View Paper: https://www.semanticscholar.org/paper/e56ec4e8efdf899ae7c955284996b61066657f63
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In Geophysics
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- Yingjie Yang
- Javier Fullea
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Citations in the corpus
- How Does the Continental Crust Get Really Hot (2011, background): “Radioactive decay of U, Th and K has long been recognised as an important heat source in continental crust, with typical heat-production values of 0.1–3.0 W m-3 (Vilà et al. 2010).”
- 3‐D multiobservable probabilistic inversion for the compositional and thermal structure of the lithosphere and upper mantle. I: a priori petrological information and geophysical observables (2013, background): “Likewise, although RHP of typical lithospheric rocks can vary by as much as 0 to >10 W m–3 between individual samples, regional averages (more suitable for lithospheric studies) are typically limited to RHP values <3.6 W m–3 [Vilá et al., 2010; Jaupart and Mareschal, 2011].”