Apparent episodic crustal growth arising from a smoothly evolving mantle

Research Article| May 01, 1986 Apparent episodic crustal growth arising from a smoothly evolving mantle Michael Gurnis; Michael Gurnis 1Research School of Earth Sciences, Australian National University, Canberra, A.C.T. 2600, Australia Search for other works by this author on: GSW Google Scholar Geoffrey F. Davies Geoffrey F. Davies 1Research School of Earth Sciences, Australian National University, Canberra, A.C.T. 2600, Australia Search for other works by this author on: GSW Google Scholar Geology (1986) 14 (5): 396–399. https://doi.org/10.1130/0091-7613(1986)14<396:AECGAF>2.0.CO;2 Article history first online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Michael Gurnis, Geoffrey F. Davies; Apparent episodic crustal growth arising from a smoothly evolving mantle. Geology 1986;; 14 (5): 396–399. doi: https://doi.org/10.1130/0091-7613(1986)14<396:AECGAF>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Crustal-growth curves are the same as crustal-age distributions only in the absence of crustal recycling into the mantle, and are likely to be very different for Earth. Phanerozoic crust is more elevated, on average, compared to the ancient cratons, and thus may be preferentially eroded and deposited onto the mobile ocean floor. Ultimately, this may lead to the preferential recycling of young crust into the mantle. A simplified crustal-growth model shows that preferential recycling of young crust can lead to an apparent peak in crustal growth at 2–3 Ga. Furthermore, the time dependence and uneven positioning of ocean-continent convergence (sites of contemporaneous crustal growth and removal) with respect to the continents are likely to lead to rather irregular age distributions for each individual continent, with an apparent episodicity on a scale of hundreds of millions of years. Finally, considerations of the physics of convection reveals that rapid changes in mantle temperature are strongly inhibited because of the temperature dependence of silicate rheology. Episodic global magmatism and hence episodic crustal growth are not expected from our understanding of mantle convection. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.