Earth Planet. Sci. Lett. 126, 369-377.Yoneda, A., and H. Spetzler, Temperature fluctuation and thermodynamic properties in Earth's lower mantle; an application of the complete travel time equation of state, Earth Planet. Sci. Lett., 126, (4), 369-377, 1994....
Earth & Planetary Science LettersDeschamps F, Trampert J (2004) Towards a lower mantle reference temperature and composition. Earth Planet Sci Lett 222(1):161–175Deschamps, F., and J. Trampert (2004) Towards a lower mantle reference temperature and composition. Earth Planet. Sci. Lett., ...
mantle is demonstrated; it utilizes the best set of experimental data for rocks, namely, their densities, directly determined to pressures and temperatures comparable to those in the lower mantle, together with the most dependable properties of the lower mantle: its seismic velocities and its ...
Phase Equilibria Modeling and P-T Evolution of the Mafic Lower-Crustal Xenoliths from the Southeastern Margin of the North China Craton. Journal of Earth Science, 29(5): 1236–1253. https://doi.org/10.1007/s12583-018-0849-6 Google Scholar Pawley, A. R., McMillan, P. F., Holloway, ...
The δ18O-δD relation shows that the main source is the meteoric water, together with some sedimentary water, but there are no deep magmatic water and mantle water which recharge the geothermal water in the basin. Through examining the distribution pattern of hydrogen-oxygen isotopic signatures,...
Clark C, Taylor RJM, Kylander-Clark ARC, Hacker BR (2018) Prolonged (>100 Ma) ultrahigh temperature metamorphism in the Napier Complex, East Antarctica: a petrochronological investigation of Earth’s hottest crust. J Metamorph Geol 36:1117–1139 Article CAS Google Scholar Coward MP, Spencer RM...
Thermoelasticity of silicate perovskites and magnesiowüstite and its implications for the Earth’s lower mantle Thermodynamic functions at zero pressure and their relation to equations of state of minerals Accuracy of equation-of-state formulations Extrapolation of lower mantle properties to zero press...
adiabatic temperaturecore‐mantle boundary heat flowironlower mantleouter corethermal structuredoi:10.1002/9781118992487.ch2Taku TsuchiyaGeodynamics Research Center, Ehime University, Matsuyama, Ehime Prefecture, Japan Earth‐Life Science Institute, Tokyo Institute of Technology, Meguro, Tokyo, JapanKenji Kawai...
Zhang ( 2005 ), Pressure and temperature dependence of elastic wave velocity of MgSiO3 perovskite and the composition of the lower mantle , Phys. Earth Planet. Inter. , 151 , 143 – 154 .Li, B. , and J. Zhang ( 2005 ), Pressure and temperature dependence of elastic wave velocity of ...
The CMB heat flow, which is determined by the temperature gradient and conductivity in the thermal boundary layer (TBL), controls the deep Earth dynamics, such as the lower mantle basal heating, core cooling, and dynamo activity. Analyses of the temperature profiles in the LM and OC indicate ...