Research Article

Heat Flow in the Campos Sedimentary Basin and Thermal History of the Continental Margin of Southeast Brazil

Table 3

Thermal conductivity values reported in earlier studies. The names in brackets in the second column are corresponding formations in the adjacent Campos basin.

RegionLayer/formationRock typeThermal conductivity (W/m/K)

Platform area [40]Ocean floorSediments1.5–2.1

Continental part of Campos basin [41]Drill cuttingsShaly sand
Sandy shale
2.2–3.5
2.5–3.2

Campos ([63, 64]) and Espirito Santo [42] basinsRio Doce (Emborê)Shale
Sandstone
1.6
1.9
Caravelas (Ubatuba)Carbonates2.3
Urucutuca (Campos)Shale
Sandstone
1.9
2.7
Barra Nova (Macaé)Shale
Sandstone
Carbonates
1.7
2.5
3.0
Mariricu (Lagoa Feia)Shale
Sandstone
Carbonates
Anhydrite
2.4
2.8
2.9
5.7

Basement [77]PrecambrianMafics
Metamorphics
2.1
3.9