Gurnis, Michael and Davies, Geoffrey F. (1986) Apparent episodic crustal growth arising from a smoothly evolving mantle. Geology, 14 (5). pp. 396-399. ISSN 0091-7613. http://resolver.caltech.edu/CaltechAUTHORS:20121128-091207413
Full text is not posted in this repository. Consult Related URLs below.
Use this Persistent URL to link to this item: http://resolver.caltech.edu/CaltechAUTHORS:20121128-091207413
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.
|Additional Information:||© 1986 Geological Society of America. Manuscript received October 9, 1985. Revised manuscript received January 14, 1986. Manuscript accepted January 22, 1986.|
|Usage Policy:||No commercial reproduction, distribution, display or performance rights in this work are provided.|
|Deposited By:||Tony Diaz|
|Deposited On:||28 Nov 2012 17:48|
|Last Modified:||11 Jun 2015 12:59|
Repository Staff Only: item control page