Abstract
Plate tectonics is central to many aspects of the geology and evolution of terrestrial planets, yet it is only observed on the Earth while all other known planets are covered with a stagnant lithosphere. Plate motions on the Earth are mostly driven by the pull of subducting slabs, therefore understanding the initiation of subduction is crucial to understanding plate tectonics initiation. On a one-plate planet which lacks the forces due to plate motions, some other mechanisms will have to cause the first episode of subduction to mobilize the surface. Sublithospheric convection has been proposed as a possible mechanism that induce stresses in the lithosphere. The question is whether these stresses can initiate subduction. We develop scaling laws for the criterion of lithospheric failure from single-cell steady-state convection, which has more controlled flow and thus easier to analyze. We show that these scaling laws are applicable to time-dependent convection. We also investigate the time-dependent behavior of convection to understand the factors controlling the timing of lithospheric failure. We find that the variation in timing not only systematically depends on the physical parameters of the convecting mantle; for convective systems with the same set of parameters, small variations in initial conditions result in different structures of the lithosphere. This changes the stresses in the lithosphere and gives rise to different times of lithospheric failure. This study suggests that it is important to address the question of when plate tectonics can initiate on a planet, in addition to finding favorable conditions for lithospheric failure. We extrapolate the scaling laws to planetary conditions to assess the feasibility of plate tectonics for terrestrial planets, and estimate whether plate tectonics can happen in reasonable planetary lifetimes.
Committee Chair
Viatcheslav S. Solomatov
Committee Members
Ramanath Cowsik, William B. McKinnon, Philip Skemer, Douglas A. Wiens,
Degree
Doctor of Philosophy (PhD)
Author's Department
Earth & Planetary Sciences
Document Type
Dissertation
Date of Award
Spring 5-15-2016
Language
English (en)
DOI
https://doi.org/10.7936/K7NC5ZGP
Author's ORCID
https://orcid.org/0000-0002-1569-7109
Recommended Citation
Wong, Teresa, "Plate Tectonics Initiation on Earth-Like Planets: Insights From Numerical and Theoretical Analysis of Convection-Induced Lithospheric Failure" (2016). Arts & Sciences Theses and Dissertations. 768.
The definitive version is available at https://doi.org/10.7936/K7NC5ZGP
Comments
Permanent URL: https://doi.org/10.7936/K7NC5ZGP