Low mantle heat flow at the edge of the North American Continent, Voisey Bay, Labrador

• Published in: Geophysical Research Letters
• Main Authors: Mareschal, J. C., Poirier, A., Rolandone, F., Bienfait, G., Gariépy, C., Lapointe, R., Jaupart, C.
• Other Authors: Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2000
• Subjects: Tectonophysics: Dynamics of lithosphere and mantle-general; Tectonophysics: Heat generation and transport; [SDU]Sciences of the Universe [physics]; Nain; Labrador Sea
• Online Access: https://insu.hal.science/insu-03596945; https://insu.hal.science/insu-03596945v1/document; https://insu.hal.science/insu-03596945v1/file/Geophysical%20Research%20Letters%20-%202000%20-%20Mareschal%20-%20Low%20mantle%20heat%20flow%20at%20the%20edge%20of%20the%20North%20American%20Continent%20Voisey.pdf; https://doi.org/10.1029/1999GL011069

International audience Heat flow measurements in 4 deep drillholes near Voisey Bay, Labrador, have yielded the lowest value ever reported in the Canadian Shield, 22 mW m -2 . This very reliable estimate is also one of the lowest continental heat flow values world wide. It requires the crust to be very poor in radioelements in this part of the Archean Nain Province. It also strongly supports the view that mantle heat flow is low (<15 mW m -2 ) throughout the Canadian Shield, with no trend of increasing mantle heat flow near the edges of the continent. It also raises questions about the controlling mechanism for rifting and the opening of the Labrador Sea at 100 Ma.