Brazilian Curie isothermal mapping: the THERMOMAG model

Abstract Geothermally, the lithosphere can be defined as the outermost layer of the Earth in which heat is primarily transferred by conduction. It typically includes the crust and upper mantle. Crustal structural provinces are segments of the crust that have the same range of geochronologic ages and...

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Bibliographic Details
Main Authors: Suze N. P. Guimaraes, Beatriz L. de Jesus, Fábio P. Vieira
Format: Article
Language:English
Published: SpringerOpen 2024-11-01
Series:Geothermal Energy
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Online Access:https://doi.org/10.1186/s40517-024-00321-6
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