کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
6430644 | 1634804 | 2012 | 15 صفحه PDF | دانلود رایگان |

A new analysis of plate cooling models indicates that the properties of oceanic lithosphere may need to be reevaluated, or that additional phenomena beyond the conditions of simple mineral physics plate models are important. Thermal models with constant and variable mineral physics properties are formally analyzed for fits against recently filtered databases for heat flow and topography. Formalisms are developed for the evaluation of the effective properties of oceanic lithosphere and the treatment of temperature-dependent thermal conductivity and thermal expansivity as both variable and freely adjustable parameters in fitting analysis. Excellent fits to depth and heat flow are resolved for a wide range of models. Good fitting parameterizations reproduce conventional estimates of net surface heat flux (â¼31.5±1.0 TW) while the apparent thermal diffusivity is higher (â¼1.1±0.1 mm2 sâ1) and apparent thermal expansivity is lower (â¼2.4Ã10â5 Kâ1) than previous reference models. Two preferred reference models, R1 and RT1, are resolved, which are consistent with evidence of mantle temperature and plate thickness, and do not require adjustments to experimental heat transport properties.
⺠A new analysis with variable properties and updated geophysical constraints. ⺠Thermal properties explored as both temperature-dependent and free parameters. ⺠Formalisms developed for the analysis of variable thermal properties. ⺠Excellent fits to geophysical observations resolved. ⺠Best fits predict high thermal diffusivity and low thermal expansivity.
Journal: Earth and Planetary Science Letters - Volumes 333â334, 1 June 2012, Pages 250-264