Mantle temperature as a control on the time scale of thermal evolution of extensional basins

TY - JOUR

T1 - Mantle temperature as a control on the time scale of thermal evolution of extensional basins

AU - Petersen, K. D.

AU - Armitage, J. J.

AU - Nielsen, S. B.

AU - Thybo, Hans

PY - 2015/1

Y1 - 2015/1

N2 - Extension of the lithosphere, the thermo-mechanical boundary layer above the convecting mantle, is followed by cooling and subsidence. The timescale of oceanic basin subsidence is ~100 Myr whereas basins of the continental interior often subside continuously for more than 200 Myr after rifting. Using numerical modelling, we show how these diverse rifting scenarios are unified when accounting for varying mantle potential temperature. At a temperature of 1300 °C, cooling is plate-like with nearly exponential subsidence as observed in oceanic basins. At 1200 °C, subsidence is almost linear and continues for more than 800 Myr. The longevity of basin subsidence in the continental interior can therefore be explained by variation of mantle temperature. An additional cause of the longevity of subsidence is related to the equilibrium thickness of the lithosphere which is increased by the local reduction of heat producing elements due to crustal thinning. Consequently, the thermally mature lithosphere of an extensional basin can be thicker than the surrounding lithosphere. This mechanism contributes to additional thermal subsidence compared to the case where the base of the lithosphere is assumed held at a constant depth.

AB - Extension of the lithosphere, the thermo-mechanical boundary layer above the convecting mantle, is followed by cooling and subsidence. The timescale of oceanic basin subsidence is ~100 Myr whereas basins of the continental interior often subside continuously for more than 200 Myr after rifting. Using numerical modelling, we show how these diverse rifting scenarios are unified when accounting for varying mantle potential temperature. At a temperature of 1300 °C, cooling is plate-like with nearly exponential subsidence as observed in oceanic basins. At 1200 °C, subsidence is almost linear and continues for more than 800 Myr. The longevity of basin subsidence in the continental interior can therefore be explained by variation of mantle temperature. An additional cause of the longevity of subsidence is related to the equilibrium thickness of the lithosphere which is increased by the local reduction of heat producing elements due to crustal thinning. Consequently, the thermally mature lithosphere of an extensional basin can be thicker than the surrounding lithosphere. This mechanism contributes to additional thermal subsidence compared to the case where the base of the lithosphere is assumed held at a constant depth.

KW - Cratonic basins

KW - Crustal heat production

KW - Equilibrium lithosphere

KW - Rifting

KW - Small-scale mantle convection

KW - Thermal subsidence

U2 - 10.1016/j.epsl.2014.10.043

DO - 10.1016/j.epsl.2014.10.043

M3 - Journal article

AN - SCOPUS:84915747620

SN - 0012-821X

VL - 409

SP - 61

EP - 70

JO - Earth and Planetary Science Letters

JF - Earth and Planetary Science Letters

ER -