Vertical gradients of heat production in the continental crust 1. Theoretical detectability from near-surface measurements
- 10 June 1971
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 76 (17) , 3842-3851
- https://doi.org/10.1029/jb076i017p03842
Abstract
No abstract availableKeywords
This publication has 12 references indexed in Scilit:
- Geochemical investigations of deep-seated rocks in the Australian shieldPublished by Elsevier ,2006
- Estimates of the crustal abundances of thorium, uranium and potassiumPublished by Elsevier ,2003
- Crustal temperature and heat production: Implications of the linear heat-flow relationJournal of Geophysical Research, 1970
- Heat flow and radioactivity in AustraliaEarth and Planetary Science Letters, 1970
- Preliminary geothermal model of the Sierra NevadaJournal of Geophysical Research, 1968
- Heat flow and surface radioactivity measurements in the Precambrian shield of Western AustraliaPhysics of the Earth and Planetary Interiors, 1968
- The vertical distribution of uranium, thorium, and potassium in the Continental CrustGeochimica et Cosmochimica Acta, 1967
- Distribution of thorium, uranium, and potassium concentrations in three cores from the Conway Granite, New Hampshire, USAAmerican Journal of Science, 1965
- Concentration of radioactive elements in deep crustal materialGeochimica et Cosmochimica Acta, 1965
- Lognormality of thorium concentrations in the Conway graniteGeochimica et Cosmochimica Acta, 1963