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TitleThe influence of deep water cycling on plate tectonic transitions and the thermal histories of the Earth and rocky planets
AuthorFuentes, J; Crowley, J WORCID logo; Mitrovica, J X
SourceAmerican Geophysical Union Fall Meeting 2019, abstracts; DI43A-0031, 2019 p. 1 Open Access logo Open Access
LinksOnline - En ligne
Alt SeriesNatural Resources Canada, Contribution Series 20190252
PublisherAmerican Geophysical Union
MeetingAmerican Geophysical Union Fall Meeting 2019; San Francisco, CA; US; December 9-13, 2019
DocumentWeb site
Mediaon-line; digital
File formathtml; pdf
Subjectstectonics; extraterrestrial geology; Nature and Environment; Science and Technology; plate tectonics; thermal history; mantle; viscosity; convection; mid-ocean ridges; subduction zones; tectonic setting; stress analyses; plate motions; models; thermal analyses; temperature
ProgramCanadian Geodetic Survey Geodetic Analysis and Development - Gravity and heights systems
Released2019 12 01
AbstractDeep water cycling has been shown to have a strong influence on mantle dynamics in both numerical and analytic studies (e.g. Sandu et al., 2011, Nakagawa et al., 2015). Small increases in mantle water content can significantly reduce mantle viscosity and thus have a strong influence on the style of plate tectonics and the thermal evolution of the mantle. In this study, we investigate the influence of mantle water cycling on the thermal history of the Earth using the analytical mantle convection model of Crowley and O’Connell (2012) with degassing occurring at ocean ridges and regassing at subduction zones. Previous analytic models that investigate water cycling in the mantle often assume a constant scaling between the Nusselt number and the Rayleigh number, implying a constant style of plate tectonics (e.g. Sandu et al. 2011, Crowley et al., 2011, Seales and Lenardic, 2017). In contrast, the model we have developed allows for natural transitions between sluggish- and active-lid plate tectonics. Both styles are forms of mobile-lid plate tectonics; however, active-lid tectonics refers to the case where the plate is driven by stresses at the plate-mantle boundary and plate speed scales with mantle temperature, while in the sluggish-lid case the plate is driven by local internal body forces, and plate speeds tend to be much smaller than mantle speeds. The model is run forward in time from 4 Ga to present using a wide range of realistic mantle and lithospheric parameters. Results show that active-lid tectonics acts to regulate the mantle temperature and water content such that the initial values have little influence over the final values. In contrast, sluggish-lid tectonics is very sensitive to the starting conditions. Furthermore, the initial water content and temperature have a strong control on the initial tectonic state and whether transitions will occur between states.

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