Much of the first hour was spent discussing logistics and course format.
Following this we discussed the morphology of ridges and examined some
maps.
Given answeres to the above, we can then compare the dimensions and
physical characteristics of the Oman ophiolite to those expected for oceanic
crust formed at different spreading rates.
We will learn that beyond the structural evidence, there is petrologic arguments that indicate at what type of ridge the Oman ophiolite was formed.
In recent years there have been several review papers related to mid-ocean ridges. These are not required reading, however, I suggest scanning the various papers (particularly their figures) to get an idea of variability in ridge crest structure.
*Forsyth, D. W., Geophysical constraints on mantle flow and melt geneartation benat mid-ocean ridges. In Mantle Flow, Melt Generation and Lithospheric Deformation at Mid-ocean Ridges, Geophys. Mongogr., Washington, DC: AGU
Macdonald, K.C. and others, A new view of the mid-ocean ridge from the
behaviour of ridge-axis discontinuities, Nature,
335, 217-225, 1988.
*Solomon, S.C and Toomey, D.R., The structure of mid-ocean ridges,
Annu. Rev. Earth Planet. Sci., 20, 329-364,
1992.
*Indicates that a single copy of the paper or the book can be found in the foyer of Cascade 105.