High heat flow in the Trans-Hudson Orogen, central Canadian Shield

Geophysical Research Letters

Volumn 23, Issue 21, 1996, Pages 3027-3030

  Guillou Frottier, L ^a   Jaupart, C ^b   Mareschal, J C ^a   Gariepy C ^a,b   Bienfait, G ^b   Cheng, L Z ^a   Lapointe, R ^a  

^a UNIVERSITÉ DU QUÉBEC À MONTRÉAL   (Canada)

^b INSTITUT DE PHYSIQUE DU GLOBE DE PARIS   (France)

Author keywords

[No Author keywords available]

Indexed keywords

REFRACTION; GEOLOGY; GEOPHYSICS; HEAT FLUX; HEAT TRANSFER; ROCKS;

CANADIAN SHIELDS; ELASTIC THICKNESS; HEAT FLOW VALUE; HEAT PRODUCTION; QUARTZITE FORMATIONS; REFRACTION EFFECTS; THERMALLY INDUCED; TRANS-HUDSON OROGEN;

HEAT TRANSFER; TECTONICS;

CALLUNA VULGARIS;

CANADIAN SHIELD; HEAT REFRACTION EFFECTS;

CRUSTAL STRUCTURE; HEAT FLOW; LITHOLOGY; SPATIAL VARIATION;

CANADA, CANADIAN SHIELD, TRANS-HUDSON OROGEN;

EID: 0030265255     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/96GL02895     Document Type: Article

References (2)

1. Pinet, C., C. Jaupart, J-C. Mareschal, G. Gariépy, G. Bienfait and R. Lapointe, Heat flow and structure of the lithosphere in the eastern Canadian Shield, J. Geophys. Res., 96, 19941-19963, 1991.
2. Sass, J.H., A.H. Lachenbruch and A.M. Jessop, Uniform heat flow in a deep hole in the Canadian Shield and its paleoclimatic implications, J. Geophys. Res., 76, 8586-8596, 1971.